CINXE.COM

<!DOCTYPE html> <html lang="en" xmlns:fb="http://www.facebook.com/2008/fbml" class="wf-loading"> <head prefix="og: https://ogp.me/ns# fb: https://ogp.me/ns/fb# academia: https://ogp.me/ns/fb/academia#"> <meta charset="utf-8"> <meta name=viewport content="width=device-width, initial-scale=1"> <meta rel="search" type="application/opensearchdescription+xml" href="/open_search.xml" title="Academia.edu"> <title>Jitka Mikova | Czech Geological Survey - Academia.edu</title>  <link href="//a.academia-assets.com/images/favicons/favicon-production.ico" rel="shortcut icon" type="image/vnd.microsoft.icon"> <link rel="apple-touch-icon" sizes="57x57" href="//a.academia-assets.com/images/favicons/apple-touch-icon-57x57.png"> <link rel="apple-touch-icon" sizes="60x60" href="//a.academia-assets.com/images/favicons/apple-touch-icon-60x60.png"> <link rel="apple-touch-icon" sizes="72x72" href="//a.academia-assets.com/images/favicons/apple-touch-icon-72x72.png"> <link rel="apple-touch-icon" sizes="76x76" href="//a.academia-assets.com/images/favicons/apple-touch-icon-76x76.png"> <link rel="apple-touch-icon" sizes="114x114" href="//a.academia-assets.com/images/favicons/apple-touch-icon-114x114.png"> <link rel="apple-touch-icon" sizes="120x120" href="//a.academia-assets.com/images/favicons/apple-touch-icon-120x120.png"> <link rel="apple-touch-icon" sizes="144x144" href="//a.academia-assets.com/images/favicons/apple-touch-icon-144x144.png"> <link rel="apple-touch-icon" sizes="152x152" href="//a.academia-assets.com/images/favicons/apple-touch-icon-152x152.png"> <link rel="apple-touch-icon" sizes="180x180" href="//a.academia-assets.com/images/favicons/apple-touch-icon-180x180.png"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-32x32.png" sizes="32x32"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-194x194.png" sizes="194x194"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-96x96.png" sizes="96x96"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/android-chrome-192x192.png" sizes="192x192"> <link rel="icon" type="image/png" href="//a.academia-assets.com/images/favicons/favicon-16x16.png" sizes="16x16"> <link rel="manifest" href="//a.academia-assets.com/images/favicons/manifest.json"> <meta name="msapplication-TileColor" content="#2b5797"> <meta name="msapplication-TileImage" content="//a.academia-assets.com/images/favicons/mstile-144x144.png"> <meta name="theme-color" content="#ffffff"> <script> window.performance && window.performance.measure && window.performance.measure("Time To First Byte", "requestStart", "responseStart"); </script> <script> (function() { if (!window.URLSearchParams || !window.history || !window.history.replaceState) { return; } var searchParams = new URLSearchParams(window.location.search); var paramsToDelete = [ 'fs', 'sm', 'swp', 'iid', 'nbs', 'rcc', // related content category 'rcpos', // related content carousel position 'rcpg', // related carousel page 'rchid', // related content hit id 'f_ri', // research interest id, for SEO tracking 'f_fri', // featured research interest, for SEO tracking (param key without value) 'f_rid', // from research interest directory for SEO tracking 'f_loswp', // from research interest pills on LOSWP sidebar for SEO tracking 'rhid', // referrring hit id ]; if (paramsToDelete.every((key) => searchParams.get(key) === null)) { return; } paramsToDelete.forEach((key) => { searchParams.delete(key); }); var cleanUrl = new URL(window.location.href); cleanUrl.search = searchParams.toString(); history.replaceState({}, document.title, cleanUrl); })(); </script> <script async src="https://www.googletagmanager.com/gtag/js?id=G-5VKX33P2DS"></script> <script> window.dataLayer = window.dataLayer || []; function gtag(){dataLayer.push(arguments);} gtag('js', new Date()); gtag('config', 'G-5VKX33P2DS', { cookie_domain: 'academia.edu', send_page_view: false, }); gtag('event', 'page_view', { 'controller': "profiles/works", 'action': "summary", 'controller_action': 'profiles/works#summary', 'logged_in': 'false', 'edge': 'unknown', // Send nil if there is no A/B test bucket, in case some records get logged // with missing data - that way we can distinguish between the two cases. // ab_test_bucket should be of the form <ab_test_name>:<bucket> 'ab_test_bucket': null, }) </script> <script type="text/javascript"> window.sendUserTiming = function(timingName) { if (!(window.performance && window.performance.measure)) return; var entries = window.performance.getEntriesByName(timingName, "measure"); if (entries.length !== 1) return; var timingValue = Math.round(entries[0].duration); gtag('event', 'timing_complete', { name: timingName, value: timingValue, event_category: 'User-centric', }); }; window.sendUserTiming("Time To First Byte"); </script> <meta name="csrf-param" content="authenticity_token" /> <meta name="csrf-token" content="r7nJlK5Ex8b3GYILp19AvDAuEmgHe55JgFhtFRlBH0QBlB97HyIFW1y0II2jXGSLb4EdV9I91yqJZtWotanBXA==" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/wow-77f7b87cb1583fc59aa8f94756ebfe913345937eb932042b4077563bebb5fb4b.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/social/home-9e8218e1301001388038e3fc3427ed00d079a4760ff7745d1ec1b2d59103170a.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/heading-b2b823dd904da60a48fd1bfa1defd840610c2ff414d3f39ed3af46277ab8df3b.css" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/button-3cea6e0ad4715ed965c49bfb15dedfc632787b32ff6d8c3a474182b231146ab7.css" /><link crossorigin="" href="https://fonts.gstatic.com/" rel="preconnect" /><link href="https://fonts.googleapis.com/css2?family=DM+Sans:ital,opsz,wght@0,9..40,100..1000;1,9..40,100..1000&family=Gupter:wght@400;500;700&family=IBM+Plex+Mono:wght@300;400&family=Material+Symbols+Outlined:opsz,wght,FILL,GRAD@20,400,0,0&display=swap" rel="stylesheet" /><link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system/common-10fa40af19d25203774df2d4a03b9b5771b45109c2304968038e88a81d1215c5.css" /> <meta name="author" content="jitka mikova" /> <meta name="description" content="Jitka Mikova, Czech Geological Survey: 23 Followers, 8 Following, 77 Research papers. Research interest: Geochemistry." /> <meta name="google-site-verification" content="bKJMBZA7E43xhDOopFZkssMMkBRjvYERV-NaN4R6mrs" /> <script> var $controller_name = 'works'; var $action_name = "summary"; var $rails_env = 'production'; var $app_rev = '9387f500ddcbb8d05c67bef28a2fe0334f1aafb8'; var $domain = 'academia.edu'; var $app_host = "academia.edu"; var $asset_host = "academia-assets.com"; var $start_time = new Date().getTime(); var $recaptcha_key = "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB"; var $recaptcha_invisible_key = "6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj"; var $disableClientRecordHit = false; </script> <script> window.Aedu = { hit_data: null }; window.Aedu.SiteStats = {"premium_universities_count":15267,"monthly_visitors":"113 million","monthly_visitor_count":113389981,"monthly_visitor_count_in_millions":113,"user_count":277786104,"paper_count":55203019,"paper_count_in_millions":55,"page_count":432000000,"page_count_in_millions":432,"pdf_count":16500000,"pdf_count_in_millions":16}; window.Aedu.serverRenderTime = new Date(1733093408000); window.Aedu.timeDifference = new Date().getTime() - 1733093408000; window.Aedu.isUsingCssV1 = false; window.Aedu.enableLocalization = true; window.Aedu.activateFullstory = false; window.Aedu.serviceAvailability = { status: {"attention_db":"on","bibliography_db":"on","contacts_db":"on","email_db":"on","indexability_db":"on","mentions_db":"on","news_db":"on","notifications_db":"on","offsite_mentions_db":"on","redshift":"on","redshift_exports_db":"on","related_works_db":"on","ring_db":"on","user_tests_db":"on"}, serviceEnabled: function(service) { return this.status[service] === "on"; }, readEnabled: function(service) { return this.serviceEnabled(service) || this.status[service] === "read_only"; }, }; window.Aedu.viewApmTrace = function() { // Check if x-apm-trace-id meta tag is set, and open the trace in APM // in a new window if it is. var apmTraceId = document.head.querySelector('meta[name="x-apm-trace-id"]'); if (apmTraceId) { var traceId = apmTraceId.content; // Use trace ID to construct URL, an example URL looks like: // https://app.datadoghq.com/apm/traces?query=trace_id%31298410148923562634 var apmUrl = 'https://app.datadoghq.com/apm/traces?query=trace_id%3A' + traceId; window.open(apmUrl, '_blank'); } }; </script>  <link href="https://fonts.googleapis.com/css?family=Roboto:100,100i,300,300i,400,400i,500,500i,700,700i,900,900i" rel="stylesheet"> <link href="//maxcdn.bootstrapcdn.com/font-awesome/4.3.0/css/font-awesome.min.css" rel="stylesheet"> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/libraries-a9675dcb01ec4ef6aa807ba772c7a5a00c1820d3ff661c1038a20f80d06bb4e4.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/academia-bdb9e8c097f01e611f2fc5e2f1a9dc599beede975e2ae5629983543a1726e947.css" /> <link rel="stylesheet" media="all" href="//a.academia-assets.com/assets/design_system_legacy-056a9113b9a0f5343d013b29ee1929d5a18be35fdcdceb616600b4db8bd20054.css" /> <script src="//a.academia-assets.com/assets/webpack_bundles/runtime-bundle-005434038af4252ca37c527588411a3d6a0eabb5f727fac83f8bbe7fd88d93bb.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/webpack_libraries_and_infrequently_changed.wjs-bundle-3e572e3b706c3ed2ec5b2c1cb44a411fadc81f62a97963cb7bd9c327a0a9d5f2.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/core_webpack.wjs-bundle-2e8d3f30eaaddd1debd6ce4630b3453b23a23c91ac7c823ddf8822879835b029.js"></script> <script src="//a.academia-assets.com/assets/webpack_bundles/sentry.wjs-bundle-5fe03fddca915c8ba0f7edbe64c194308e8ce5abaed7bffe1255ff37549c4808.js"></script> <script> jade = window.jade || {}; jade.helpers = window.$h; jade._ = window._; </script>  <script id="tag-manager-head-root">(function(w,d,s,l,i){w[l]=w[l]||[];w[l].push({'gtm.start': new Date().getTime(),event:'gtm.js'});var f=d.getElementsByTagName(s)[0], j=d.createElement(s),dl=l!='dataLayer'?'&l='+l:'';j.async=true;j.src= 'https://www.googletagmanager.com/gtm.js?id='+i+dl;f.parentNode.insertBefore(j,f); })(window,document,'script','dataLayer_old','GTM-5G9JF7Z');</script>  <script> window.gptadslots = []; window.googletag = window.googletag || {}; window.googletag.cmd = window.googletag.cmd || []; </script> <script type="text/javascript"> // TODO(jacob): This should be defined, may be rare load order problem. // Checking if null is just a quick fix, will default to en if unset. // Better fix is to run this immedietely after I18n is set. if (window.I18n != null) { I18n.defaultLocale = "en"; I18n.locale = "en"; I18n.fallbacks = true; } </script> <link rel="canonical" href="https://czechgeologicalsurvey.academia.edu/JitkaMikova" /> </head>   <body class='c-profiles/works a-summary logged_out'>  <div id="fb-root"></div><script>window.fbAsyncInit = function() { FB.init({ appId: "2369844204", version: "v8.0", status: true, cookie: true, xfbml: true }); // Additional initialization code. if (window.InitFacebook) { // facebook.ts already loaded, set it up. window.InitFacebook(); } else { // Set a flag for facebook.ts to find when it loads. window.academiaAuthReadyFacebook = true; } };</script><script>window.fbAsyncLoad = function() { // Protection against double calling of this function if (window.FB) { return; } (function(d, s, id){ var js, fjs = d.getElementsByTagName(s)[0]; if (d.getElementById(id)) {return;} js = d.createElement(s); js.id = id; js.src = "//connect.facebook.net/en_US/sdk.js"; fjs.parentNode.insertBefore(js, fjs); }(document, 'script', 'facebook-jssdk')); } if (!window.defer_facebook) { // Autoload if not deferred window.fbAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.fbAsyncLoad(); }, 5000); }</script> <div id="google-root"></div><script>window.loadGoogle = function() { if (window.InitGoogle) { // google.ts already loaded, set it up. window.InitGoogle("331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"); } else { // Set a flag for google.ts to use when it loads. window.GoogleClientID = "331998490334-rsn3chp12mbkiqhl6e7lu2q0mlbu0f1b"; } };</script><script>window.googleAsyncLoad = function() { // Protection against double calling of this function (function(d) { var js; var id = 'google-jssdk'; var ref = d.getElementsByTagName('script')[0]; if (d.getElementById(id)) { return; } js = d.createElement('script'); js.id = id; js.async = true; js.onload = loadGoogle; js.src = "https://accounts.google.com/gsi/client" ref.parentNode.insertBefore(js, ref); }(document)); } if (!window.defer_google) { // Autoload if not deferred window.googleAsyncLoad(); } else { // Defer loading by 5 seconds setTimeout(function() { window.googleAsyncLoad(); }, 5000); }</script> <div id="tag-manager-body-root">  <noscript><iframe src="https://www.googletagmanager.com/ns.html?id=GTM-5G9JF7Z" height="0" width="0" style="display:none;visibility:hidden"></iframe></noscript>   <script> window.addEventListener('load', function() { if (document.querySelector('input[name="commit"]')) { document.querySelector('input[name="commit"]').addEventListener('click', function() { gtag('event', 'click', { event_category: 'button', event_label: 'Log In' }) }) } }); </script> </div> <script>var _comscore = _comscore || []; _comscore.push({ c1: "2", c2: "26766707" }); (function() { var s = document.createElement("script"), el = document.getElementsByTagName("script")[0]; s.async = true; s.src = (document.location.protocol == "https:" ? "https://sb" : "http://b") + ".scorecardresearch.com/beacon.js"; el.parentNode.insertBefore(s, el); })();</script><img src="https://sb.scorecardresearch.com/p?c1=2&c2=26766707&cv=2.0&cj=1" style="position: absolute; visibility: hidden" /> <div id='react-modal'></div> <div class='DesignSystem'> <a class='u-showOnFocus' href='#site'> Skip to main content </a> </div> <div id="upgrade_ie_banner" style="display: none;"><p>Academia.edu no longer supports Internet Explorer.</p><p>To browse Academia.edu and the wider internet faster and more securely, please take a few seconds to <a href="https://www.academia.edu/upgrade-browser">upgrade your browser</a>.</p></div><script>// Show this banner for all versions of IE if (!!window.MSInputMethodContext || /(MSIE)/.test(navigator.userAgent)) { document.getElementById('upgrade_ie_banner').style.display = 'block'; }</script> <div class="DesignSystem bootstrap ShrinkableNav"><div class="navbar navbar-default main-header"><div class="container-wrapper" id="main-header-container"><div class="container"><div class="navbar-header"><div class="nav-left-wrapper u-mt0x"><div class="nav-logo"><a data-main-header-link-target="logo_home" href="https://www.academia.edu/"><img class="visible-xs-inline-block" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015-A.svg" width="24" height="24" /><img width="145.2" height="18" class="hidden-xs" style="height: 24px;" alt="Academia.edu" src="//a.academia-assets.com/images/academia-logo-redesign-2015.svg" /></a></div><div class="nav-search"><div class="SiteSearch-wrapper select2-no-default-pills"><form class="js-SiteSearch-form DesignSystem" action="https://www.academia.edu/search" accept-charset="UTF-8" method="get"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><i class="SiteSearch-icon fa fa-search u-fw700 u-positionAbsolute u-tcGrayDark"></i><input class="js-SiteSearch-form-input SiteSearch-form-input form-control" data-main-header-click-target="search_input" name="q" placeholder="Search" type="text" value="" /></form></div></div></div><div class="nav-right-wrapper pull-right"><ul class="NavLinks js-main-nav list-unstyled"><li class="NavLinks-link"><a class="js-header-login-url Button Button--inverseGray Button--sm u-mb4x" id="nav_log_in" rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="NavLinks-link u-p0x"><a class="Button Button--inverseGray Button--sm u-mb4x" rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li></ul><button class="hidden-lg hidden-md hidden-sm u-ml4x navbar-toggle collapsed" data-target=".js-mobile-header-links" data-toggle="collapse" type="button"><span class="icon-bar"></span><span class="icon-bar"></span><span class="icon-bar"></span></button></div></div><div class="collapse navbar-collapse js-mobile-header-links"><ul class="nav navbar-nav"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/login">Log In</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/signup">Sign Up</a></li><li class="u-borderColorGrayLight u-borderBottom1 js-mobile-nav-expand-trigger"><a href="#">more&nbsp<span class="caret"></span></a></li><li><ul class="js-mobile-nav-expand-section nav navbar-nav u-m0x collapse"><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/about">About</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/press">Press</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://medium.com/@academia">Blog</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="false" href="https://www.academia.edu/documents">Papers</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://www.academia.edu/hiring"><i class="fa fa-briefcase"></i> We're Hiring!</a></li><li class="u-borderColorGrayLight u-borderBottom1"><a rel="nofollow" href="https://support.academia.edu/"><i class="fa fa-question-circle"></i> Help Center</a></li><li class="js-mobile-nav-collapse-trigger u-borderColorGrayLight u-borderBottom1 dropup" style="display:none"><a href="#">less&nbsp<span class="caret"></span></a></li></ul></li></ul></div></div></div><script>(function(){ var $moreLink = $(".js-mobile-nav-expand-trigger"); var $lessLink = $(".js-mobile-nav-collapse-trigger"); var $section = $('.js-mobile-nav-expand-section'); $moreLink.click(function(ev){ ev.preventDefault(); $moreLink.hide(); $lessLink.show(); $section.collapse('show'); }); $lessLink.click(function(ev){ ev.preventDefault(); $moreLink.show(); $lessLink.hide(); $section.collapse('hide'); }); })() if ($a.is_logged_in() || false) { new Aedu.NavigationController({ el: '.js-main-nav', showHighlightedNotification: false }); } else { $(".js-header-login-url").attr("href", $a.loginUrlWithRedirect()); } Aedu.autocompleteSearch = new AutocompleteSearch({el: '.js-SiteSearch-form'});</script></div></div> <div id='site' class='fixed'> <div id="content" class="clearfix"> <script>document.addEventListener('DOMContentLoaded', function(){ var $dismissible = $(".dismissible_banner"); $dismissible.click(function(ev) { $dismissible.hide(); }); });</script> <script src="//a.academia-assets.com/assets/webpack_bundles/profile.wjs-bundle-ae3d0ee232cd83d11499343688b0160a3c7db15e95cb2d0844cae78d49ea53f1.js" defer="defer"></script><script>Aedu.rankings = { showPaperRankingsLink: false } $viewedUser = Aedu.User.set_viewed( {"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova","photo":"/images/s65_no_pic.png","has_photo":false,"department":{"id":416844,"name":"Geochemistry","url":"https://czechgeologicalsurvey.academia.edu/Departments/Geochemistry/Documents","university":{"id":23491,"name":"Czech Geological Survey","url":"https://czechgeologicalsurvey.academia.edu/"}},"position":"Department Member","position_id":4,"is_analytics_public":false,"interests":[{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"}]} ); if ($a.is_logged_in() && $viewedUser.is_current_user()) { $('body').addClass('profile-viewed-by-owner'); } $socialProfiles = []</script><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://czechgeologicalsurvey.academia.edu/JitkaMikova","location":"/JitkaMikova","scheme":"https","host":"czechgeologicalsurvey.academia.edu","port":null,"pathname":"/JitkaMikova","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="ProfileCheckPaperUpdate" data-props="{}" data-trace="false" data-dom-id="ProfileCheckPaperUpdate-react-component-6cfc5416-a14f-42f6-ae32-b947153337f1"></div> <div id="ProfileCheckPaperUpdate-react-component-6cfc5416-a14f-42f6-ae32-b947153337f1"></div> <div class="DesignSystem"><div class="onsite-ping" id="onsite-ping"></div></div><div class="profile-user-info DesignSystem"><div class="social-profile-container"><div class="left-panel-container"><div class="user-info-component-wrapper"><div class="user-summary-cta-container"><div class="user-summary-container"><div class="social-profile-avatar-container"><img class="profile-avatar u-positionAbsolute" border="0" alt="" src="//a.academia-assets.com/images/s200_no_pic.png" /></div><div class="title-container"><h1 class="ds2-5-heading-sans-serif-sm">Jitka Mikova</h1><div class="affiliations-container fake-truncate js-profile-affiliations"><div><a class="u-tcGrayDarker" href="https://czechgeologicalsurvey.academia.edu/">Czech Geological Survey</a>, <a class="u-tcGrayDarker" href="https://czechgeologicalsurvey.academia.edu/Departments/Geochemistry/Documents">Geochemistry</a>, <span class="u-tcGrayDarker">Department Member</span></div></div></div></div><div class="sidebar-cta-container"><button class="ds2-5-button hidden profile-cta-button grow js-profile-follow-button" data-broccoli-component="user-info.follow-button" data-click-track="profile-user-info-follow-button" data-follow-user-fname="Jitka" data-follow-user-id="3753617" data-follow-user-source="profile_button" data-has-google="false"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">add</span>Follow</button><button class="ds2-5-button hidden profile-cta-button grow js-profile-unfollow-button" data-broccoli-component="user-info.unfollow-button" data-click-track="profile-user-info-unfollow-button" data-unfollow-user-id="3753617"><span class="material-symbols-outlined" style="font-size: 20px" translate="no">done</span>Following</button></div></div><div class="user-stats-container"><a><div class="stat-container js-profile-followers"><p class="label">Followers</p><p class="data">23</p></div></a><a><div class="stat-container js-profile-followees" data-broccoli-component="user-info.followees-count" data-click-track="profile-expand-user-info-following"><p class="label">Following</p><p class="data">8</p></div></a><a><div class="stat-container js-profile-coauthors" data-broccoli-component="user-info.coauthors-count" data-click-track="profile-expand-user-info-coauthors"><p class="label">Co-authors</p><p class="data">6</p></div></a><span><div class="stat-container"><p class="label"><span class="js-profile-total-view-text">Public Views</span></p><p class="data"><span class="js-profile-view-count"></span></p></div></span></div><div class="ri-section"><div class="ri-section-header"><span>Interests</span></div><div class="ri-tags-container"><a data-click-track="profile-user-info-expand-research-interests" data-has-card-for-ri-list="3753617" href="https://www.academia.edu/Documents/in/Geochemistry"><div id="js-react-on-rails-context" style="display:none" data-rails-context="{"inMailer":false,"i18nLocale":"en","i18nDefaultLocale":"en","href":"https://czechgeologicalsurvey.academia.edu/JitkaMikova","location":"/JitkaMikova","scheme":"https","host":"czechgeologicalsurvey.academia.edu","port":null,"pathname":"/JitkaMikova","search":null,"httpAcceptLanguage":null,"serverSide":false}"></div> <div class="js-react-on-rails-component" style="display:none" data-component-name="Pill" data-props="{"color":"gray","children":["Geochemistry"]}" data-trace="false" data-dom-id="Pill-react-component-cb74fac1-0c58-4ea3-94a4-2f1ee1a0765e"></div> <div id="Pill-react-component-cb74fac1-0c58-4ea3-94a4-2f1ee1a0765e"></div> </a></div></div></div></div><div class="right-panel-container"><div class="user-content-wrapper"><div class="uploads-container" id="social-redesign-work-container"><div class="upload-header"><h2 class="ds2-5-heading-sans-serif-xs">Uploads</h2></div><div class="documents-container backbone-social-profile-documents" style="width: 100%;"><div class="u-taCenter"></div><div class="profile--tab_content_container js-tab-pane tab-pane active" id="all"><div class="profile--tab_heading_container js-section-heading" data-section="Papers" id="Papers"><h3 class="profile--tab_heading_container">Papers by Jitka Mikova</h3></div><div class="js-work-strip profile--work_container" data-work-id="119267774"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge"><img alt="Research paper thumbnail of Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge" class="work-thumbnail" src="https://attachments.academia-assets.com/114677499/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge">Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge</a></div><div class="wp-workCard_item"><span>Journal of Structural Geology</span><span>, 2017</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e65a6d76dfbe9de31751fdf6322750d8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677499,"asset_id":119267774,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267774"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267774"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267774; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267774]").text(description); $(".js-view-count[data-work-id=119267774]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267774; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267774']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267774, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "e65a6d76dfbe9de31751fdf6322750d8" } } $('.js-work-strip[data-work-id=119267774]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267774,"title":"Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"New approach involving evaluation of anisotropy of magnetic susceptibility (AMS) data in stereoplots and Jelinek's P j-T space, Vollmer's eigenvalue and microstructural analyses is proposed to discriminate between homogeneous and superposed deformation in granites. This method is used to decipher the internal AMS fabric and microstructural evolution of a folded array of granitic sills. The studied major sill shows a fabric and microstructural zonality marked by submagmatic and high-temperature Type I planar-linear fabric developed at sill margins, and the transpositional Type II subsolidus fabrics that formed at high to medium temperatures deformation in the sill core. While Type I fabric is associated with dip slip magnetic lineations, Type II subsolidus fabrics are marked by subhorizontal","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Journal of Structural Geology","grobid_abstract_attachment_id":114677499},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge","translated_internal_url":"","created_at":"2024-05-17T23:06:34.160-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677499,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677499/thumbnails/1.jpg","file_name":"j.jsg.2016.11.00720240518-1-obyqzb.pdf","download_url":"https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Magnetic_fabric_transposition_in_folded.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677499/j.jsg.2016.11.00720240518-1-obyqzb-libre.pdf?1716019973=\u0026response-content-disposition=attachment%3B+filename%3DMagnetic_fabric_transposition_in_folded.pdf\u0026Expires=1733072613\u0026Signature=AWPWWapcuGjyhBpUI1MNX674TuU0cOQe~x6d3kCxFGZcdzjfSlH3s1t2VMlemnSk7FjkJEpan0KMUAaXwK5rBRHkj6UvmGeJfAVDDI~uHr82od~RPIuOvQ7VOM2p9m-y7TWyv4Xo9iBgLsJ89288X6MxI3YlG0nMiCAy4CfEaygFMmH2~NQC-FI6ZMgKHG-Mq7D3NOj0FUHFjd800yGqUoEds7lZVcPpC2m~BMaX7VST-LABij0RMkdEX4NJMy4x6QZqgBbIDH2qbbLj6D0DtX58uZjeisQxy2Tpow2X5SHqtFY0-6TOfhZFVuKOXqrmhWsOrDaYK51L9Rzg0MgABg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge","translated_slug":"","page_count":57,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677499,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677499/thumbnails/1.jpg","file_name":"j.jsg.2016.11.00720240518-1-obyqzb.pdf","download_url":"https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Magnetic_fabric_transposition_in_folded.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677499/j.jsg.2016.11.00720240518-1-obyqzb-libre.pdf?1716019973=\u0026response-content-disposition=attachment%3B+filename%3DMagnetic_fabric_transposition_in_folded.pdf\u0026Expires=1733072613\u0026Signature=AWPWWapcuGjyhBpUI1MNX674TuU0cOQe~x6d3kCxFGZcdzjfSlH3s1t2VMlemnSk7FjkJEpan0KMUAaXwK5rBRHkj6UvmGeJfAVDDI~uHr82od~RPIuOvQ7VOM2p9m-y7TWyv4Xo9iBgLsJ89288X6MxI3YlG0nMiCAy4CfEaygFMmH2~NQC-FI6ZMgKHG-Mq7D3NOj0FUHFjd800yGqUoEds7lZVcPpC2m~BMaX7VST-LABij0RMkdEX4NJMy4x6QZqgBbIDH2qbbLj6D0DtX58uZjeisQxy2Tpow2X5SHqtFY0-6TOfhZFVuKOXqrmhWsOrDaYK51L9Rzg0MgABg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":1419,"name":"Structural Geology","url":"https://www.academia.edu/Documents/in/Structural_Geology"},{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology"},{"id":197590,"name":"Sill","url":"https://www.academia.edu/Documents/in/Sill"}],"urls":[{"id":42065182,"url":"https://doi.org/10.1016/j.jsg.2016.11.007"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267773"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160"><img alt="Research paper thumbnail of Hybridization of magmas by break down of partially molten granitic rock and its assimilation&amp;#160" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160">Hybridization of magmas by break down of partially molten granitic rock and its assimilation&amp;#160</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;amp;lt;p&amp;amp;amp;gt;During orogenic processes continental crust experiences signific...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">&amp;amp;amp;lt;p&amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg&amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg&amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg&amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg&amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330&amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310&amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg&amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.&amp;amp;amp;lt;/p&amp;amp;amp;gt;</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267773"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267773"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267773; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267773]").text(description); $(".js-view-count[data-work-id=119267773]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267773; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267773']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267773, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267773]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267773,"title":"Hybridization of magmas by break down of partially molten granitic rock and its assimilation\u0026amp;#160","translated_title":"","metadata":{"abstract":"\u0026amp;amp;amp;lt;p\u0026amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg\u0026amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg\u0026amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg\u0026amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg\u0026amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330\u0026amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310\u0026amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg\u0026amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.\u0026amp;amp;amp;lt;/p\u0026amp;amp;amp;gt;","publication_date":{"day":27,"month":3,"year":2022,"errors":{}}},"translated_abstract":"\u0026amp;amp;amp;lt;p\u0026amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg\u0026amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg\u0026amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg\u0026amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg\u0026amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330\u0026amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310\u0026amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg\u0026amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.\u0026amp;amp;amp;lt;/p\u0026amp;amp;amp;gt;","internal_url":"https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160","translated_internal_url":"","created_at":"2024-05-17T23:06:33.940-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":197592,"name":"Magma","url":"https://www.academia.edu/Documents/in/Magma"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":415323,"name":"Phenocryst","url":"https://www.academia.edu/Documents/in/Phenocryst"},{"id":2601101,"name":"Granulite","url":"https://www.academia.edu/Documents/in/Granulite"},{"id":3382937,"name":"felsic","url":"https://www.academia.edu/Documents/in/felsic"}],"urls":[{"id":42065181,"url":"https://doi.org/10.5194/egusphere-egu22-2449"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267772"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation"><img alt="Research paper thumbnail of LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation">LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;lt;p&amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observati...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">&amp;amp;lt;p&amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation&amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 &amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600&amp;amp;amp;#8211;625 &amp;amp;amp;#176;C and 1.6&amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 &amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. &amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian&amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.&amp;amp;lt;/p&amp;amp;gt;</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267772"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267772"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267772; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267772]").text(description); $(".js-view-count[data-work-id=119267772]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267772; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267772']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267772, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267772]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267772,"title":"LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation","translated_title":"","metadata":{"abstract":"\u0026amp;amp;lt;p\u0026amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation\u0026amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 \u0026amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600\u0026amp;amp;amp;#8211;625 \u0026amp;amp;amp;#176;C and 1.6\u0026amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 \u0026amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. \u0026amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian\u0026amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.\u0026amp;amp;lt;/p\u0026amp;amp;gt;","publication_date":{"day":28,"month":3,"year":2022,"errors":{}}},"translated_abstract":"\u0026amp;amp;lt;p\u0026amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation\u0026amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 \u0026amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600\u0026amp;amp;amp;#8211;625 \u0026amp;amp;amp;#176;C and 1.6\u0026amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 \u0026amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. \u0026amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian\u0026amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.\u0026amp;amp;lt;/p\u0026amp;amp;gt;","internal_url":"https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation","translated_internal_url":"","created_at":"2024-05-17T23:06:33.735-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":1590367,"name":"Monazite","url":"https://www.academia.edu/Documents/in/Monazite"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065180,"url":"https://doi.org/10.5194/egusphere-egu22-9227"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267771"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_"><img alt="Research paper thumbnail of Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_">Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267771"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267771"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267771; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267771]").text(description); $(".js-view-count[data-work-id=119267771]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267771; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267771']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267771, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267771]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267771,"title":"Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":2007,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_","translated_internal_url":"","created_at":"2024-05-17T23:06:33.535-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":2601101,"name":"Granulite","url":"https://www.academia.edu/Documents/in/Granulite"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065179,"url":"https://uni-salzburg.elsevierpure.com/en/publications/potassic-granulites-from-the-blansky-les-massif-moldanubian-zone-"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267770"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_"><img alt="Research paper thumbnail of Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_">Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]</a></div><div class="wp-workCard_item"><span>Gondwana Research</span><span>, Dec 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267770"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267770"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267770; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267770]").text(description); $(".js-view-count[data-work-id=119267770]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267770; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267770']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267770, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267770]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267770,"title":"Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":12,"year":2023,"errors":{}},"publication_name":"Gondwana Research"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_","translated_internal_url":"","created_at":"2024-05-17T23:06:33.265-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"}],"urls":[{"id":42065178,"url":"https://doi.org/10.1016/j.gr.2023.06.016"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267769"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa"><img alt="Research paper thumbnail of U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa">U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267769"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267769"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267769; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267769]").text(description); $(".js-view-count[data-work-id=119267769]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267769; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267769']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267769, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267769]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267769,"title":"U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa","translated_title":"","metadata":{"publication_date":{"day":28,"month":3,"year":2022,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa","translated_internal_url":"","created_at":"2024-05-17T23:06:32.850-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065177,"url":"https://doi.org/10.5194/egusphere-egu22-12505"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267768"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone"><img alt="Research paper thumbnail of Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/114677454/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone">Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone</a></div><div class="wp-workCard_item"><span>Tectonics</span><span>, Aug 1, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c59b21ed364b99116d1b5f1c67e17b56" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677454,"asset_id":119267768,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267768"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267768"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267768; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267768]").text(description); $(".js-view-count[data-work-id=119267768]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267768; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267768']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267768, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c59b21ed364b99116d1b5f1c67e17b56" } } $('.js-work-strip[data-work-id=119267768]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267768,"title":"Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Paleozoic Geodynamics of Mongolian Altai Accretionary Wedge","grobid_abstract":"An important component of all accretionary systems is the up to 20 km-thick volcanic-sedimentary wedge built above the subducting plate, in front of a magmatic arc and upper plate continent (Cawood et al., 2009). This wedge, often several thousand kilometers long and hundreds of kilometers wide, is accreted during the ca. 100 Ma lifetime of oceanic spreading and subduction (Kusky et al., 2013). The main wedge feature is the so-called ocean plate stratigraphy with the oldest pillow lavas, bedded cherts, deep marine siliceous fine-grained sediments, and the youngest turbidites derived from a continent and magmatic arc. This sequence is often imbricated together with seamount volcanic products, and is later intruded by an oceanward migrating magmatic arc due to a continuous rollback of a subducting plate. The entire process produces a typical lithological association of Pacific-type active margins (Collins, 2002). Based on this, a classical Japan Islands-type scenario was proposed for the volcano-sedimentary accretionary prism of the Mongolian Altai Zone, one of the main constituents of the Mongolian Collage System (Long et al., 2007; Xiao, Kusky, et al., 2015). The Mongolian Altai Zone consists mainly of thick late Cambrian and Ordovician sedimentary packages covered by Silurian and Devonian volcano-clastic sequences (","publication_date":{"day":1,"month":8,"year":2022,"errors":{}},"publication_name":"Tectonics","grobid_abstract_attachment_id":114677454},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone","translated_internal_url":"","created_at":"2024-05-17T23:06:32.653-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677454,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677454/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677454/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=ASNhunF-wCYXT-4a79lxGZw7lRkQfpog0aRlFK5P2F5k7YEQfGItOTlqseZMGVjPiH58py2ABxE-1r41xHwO6dmldZrl8p8ZDbaGfrtK9hkC96fHTWbczBLylwOMgCn8Q0EIzrwQqGJbe1k6JQL6dPSwmES1-RCpC8kKnJAYd~kDVosHvJ7AdgfuoLFfqCda8IoVr7thQgF~whp2KZUdDI8QaOrmrFczD15lK8VNEi-DLTERJz7e4Mpu4vAwdPZs4pwkZRi0nIVU1PBG8NK7DEmlvqQ2ID3Q9n-zhlMnnm4NKLKQGi5ecrcOIOykuMEXEx~Z2mQ4GFQZZeWeasATgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone","translated_slug":"","page_count":36,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677454,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677454/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677454/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=ASNhunF-wCYXT-4a79lxGZw7lRkQfpog0aRlFK5P2F5k7YEQfGItOTlqseZMGVjPiH58py2ABxE-1r41xHwO6dmldZrl8p8ZDbaGfrtK9hkC96fHTWbczBLylwOMgCn8Q0EIzrwQqGJbe1k6JQL6dPSwmES1-RCpC8kKnJAYd~kDVosHvJ7AdgfuoLFfqCda8IoVr7thQgF~whp2KZUdDI8QaOrmrFczD15lK8VNEi-DLTERJz7e4Mpu4vAwdPZs4pwkZRi0nIVU1PBG8NK7DEmlvqQ2ID3Q9n-zhlMnnm4NKLKQGi5ecrcOIOykuMEXEx~Z2mQ4GFQZZeWeasATgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677455,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677455/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677455/download_file","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677455/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=SNK2HbP~fMDtoy29Wk8u37P88mq38CtEtfp-WJZVz8vA~q2lc7doN3644TQGXOZOMjCbBjNlQj9csaSzYoeRoMvYvVLCL8qlBs1BXpbp-xoyO0zNtDdjDUMwCi915pZDqeUzBusmngRUvz1OgZ~GY3d5EeUmskItq3672mO-a~BehatOLzM5xs0ytXBWxDSaFdI4IgA3B3XPh0nTTJK45ag4vq8LhqqR5DRxz1ogkOP1QIcsrQMWOdhc8TayNTHKjKUZ4iYiv~jGRf2Uz9ph41de3CeUsQahmvfHrgfWKXRnxamQsP7hdR0zxXcUybUHwSrWTRcPibQKzP60Ju~ngQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":101506,"name":"Permian","url":"https://www.academia.edu/Documents/in/Permian"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"}],"urls":[{"id":42065176,"url":"http://diposit.ub.edu/dspace/bitstream/2445/188707/1/724585.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267767"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications"><img alt="Research paper thumbnail of U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications" class="work-thumbnail" src="https://attachments.academia-assets.com/114677457/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications">U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications</a></div><div class="wp-workCard_item"><span>Gondwana Research</span><span>, May 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c607c5d2009dada2bf684a89c0bbb8a1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677457,"asset_id":119267767,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267767"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267767"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267767; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267767]").text(description); $(".js-view-count[data-work-id=119267767]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267767; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267767']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267767, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c607c5d2009dada2bf684a89c0bbb8a1" } } $('.js-work-strip[data-work-id=119267767]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267767,"title":"U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.","publication_date":{"day":1,"month":5,"year":2023,"errors":{}},"publication_name":"Gondwana Research","grobid_abstract_attachment_id":114677457},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications","translated_internal_url":"","created_at":"2024-05-17T23:06:32.427-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677457,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677457/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677457/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=E~y7Ty35U0E1npJWfFIRMPsWFZNOvPjfLCR7TBiXlwhIGqhHUccKbRLksQhbqhL2w4xt8c1SOtTcQRcmaX9atUB3BVq9s5CNA8C9Pi1snNAbsQPggKj6Ad38V-3vuZ~maSvvuXbE64p0C3NtEWAmUnEfzBoxc877tjT7VbRorwb4W5FeRxsAst5d~4kIH-4Zvzq5TtqQMvgWGcWIjtIiIgwGvFQ8fLF40UD-hg1jwhZCwtViSsWMERuIk5JE-YAjwtg14zD0TqQGedmlZ5baW8dOc9v16UNE5MJMOCXMPS8B~KqwK4sKqjie-5tJeeQwPegN7Z-LnqAx8pUXGeJlhg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications","translated_slug":"","page_count":55,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677457,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677457/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677457/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=E~y7Ty35U0E1npJWfFIRMPsWFZNOvPjfLCR7TBiXlwhIGqhHUccKbRLksQhbqhL2w4xt8c1SOtTcQRcmaX9atUB3BVq9s5CNA8C9Pi1snNAbsQPggKj6Ad38V-3vuZ~maSvvuXbE64p0C3NtEWAmUnEfzBoxc877tjT7VbRorwb4W5FeRxsAst5d~4kIH-4Zvzq5TtqQMvgWGcWIjtIiIgwGvFQ8fLF40UD-hg1jwhZCwtViSsWMERuIk5JE-YAjwtg14zD0TqQGedmlZ5baW8dOc9v16UNE5MJMOCXMPS8B~KqwK4sKqjie-5tJeeQwPegN7Z-LnqAx8pUXGeJlhg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677458,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677458/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677458/download_file","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677458/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=BK-fszsiA5vpMFr1zOCLEudTReoW0aEhs8Eo5VAwP03dxmhbvnlrQONZcWVsWi4qwoviaiLNsvC107l28jY-HLXkS9ONgGQRYCeU21hvyBkWeTP3IuNLv~9JziMWgLLcUyn~X24r-ZpxMcrE-P1xNFiHF9C8~Qj4HG6op8OVsIqPPgHpxL~U-8n3XykqjlgPo-xx-4CEKfxJY9KU7~1xpq9pmz08LJyeZtRc5YArzpF1LH2sXmO3y2ulJ9rtVqPVPxlss9kbQrLjdEnGbm8RP6H87J6J2dURKanxJDepJWL9SBq4yk6KDnKVXgbszI5N7ctcYJBjiHA5IFcfyMReCA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":191873,"name":"Magmatism","url":"https://www.academia.edu/Documents/in/Magmatism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065175,"url":"https://univoak.eu/islandora/object/islandora:159433/datastream/PDF/view"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267766"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile"><img alt="Research paper thumbnail of Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile" class="work-thumbnail" src="https://attachments.academia-assets.com/114677501/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile">Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile</a></div><div class="wp-workCard_item"><span>Applied Geochemistry</span><span>, Nov 1, 2020</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="22f0e43b5f9374c56a9ecd526fd86286" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677501,"asset_id":119267766,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267766"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267766"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267766; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267766]").text(description); $(".js-view-count[data-work-id=119267766]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267766; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267766']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267766, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "22f0e43b5f9374c56a9ecd526fd86286" } } $('.js-work-strip[data-work-id=119267766]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267766,"title":"Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Aims of the present study were to determine the extent of the uptake of selected trace elements by birch (Betula pendula Roth) growing on the partly burnt coal waste pile and to evaluate isotopic fractionation of copper (Cu) zinc (Zn). Substrates, birch sap and leaves were collected in the coal waste pile and in a reference area outside the waste pile. The concentration of trace elements in birch sap and leaves both in birch growing on the coal waste pile and at reference sites increase in the range of U, As, Se \u003e Cd, Mo, Cu \u003e Pb \u003e Ba ≫ Zn. However, the uptake of elements by birch is restricted when concentration of metals in substrates are too high. Compared to the isotopic composition of Cu in waste substrates and soils (δ 65 Cu =-0.93 to + 1.49‰), this element in sap and leaves (δ 65 Cu =-0.58 to − 1.64 and-0.59 to-2.35‰, respectively) is depleted in heavy isotope regardless of plant-available concentration of Cu in substrates. Compared to the isotopic composition of Zn in substrates (δ 66 Zn =-0.20 to 1.43‰), its isotopic composition in sap and leaves (δ 66 Zn =-0.85 to + 1.00 and-0.21 to + 0.57‰, respectively) is depleted in the heavy isotope only when the plant-available concentration of Zn in the substrate and soil is high (\u003e20 mg kg − 1). At low plant-available concentration of Zn no isotopic fractionation or enrichment of Zn in the heavy isotope was recorded.","publication_date":{"day":1,"month":11,"year":2020,"errors":{}},"publication_name":"Applied Geochemistry","grobid_abstract_attachment_id":114677501},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile","translated_internal_url":"","created_at":"2024-05-17T23:06:32.191-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677501,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677501/thumbnails/1.jpg","file_name":"j.apgeochem.2020.10474120240518-1-herkag.pdf","download_url":"https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Uptake_of_trace_elements_and_isotope_fra.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677501/j.apgeochem.2020.10474120240518-1-herkag-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DUptake_of_trace_elements_and_isotope_fra.pdf\u0026Expires=1733072613\u0026Signature=R6RB4adcwWQjvfz~DChaaqqXN639ckRpRtS0GQ3Rc4ew3sNT87UxYDW7PfSu0gu6myb9rdWCfgvACKLmJ~-m2Hmv1V~xIei8Ks~odgOE9VeqFPE48Wreb1pJcXJ~cJXC8eXpAzh1EkcTzQGk3LHpXqWjjo2fcKJrqNLXkrVx8Qw~~A8iPKt3huMq4GfTee3N9OUtC23VSypjRBtgtRSczUExxUSuJpSx1dS~1yYoCsiQI~7gZWN19-r3RzRSlGltlrJ7Zzl~kMHgbSw4RvsyuOgowGVEx0uVMoL9SpLzzFNfV9516duv~3d~pwcVBqAa1AvAr44-UdpCMYJGJOLfGQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile","translated_slug":"","page_count":14,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677501,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677501/thumbnails/1.jpg","file_name":"j.apgeochem.2020.10474120240518-1-herkag.pdf","download_url":"https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Uptake_of_trace_elements_and_isotope_fra.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677501/j.apgeochem.2020.10474120240518-1-herkag-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DUptake_of_trace_elements_and_isotope_fra.pdf\u0026Expires=1733072613\u0026Signature=R6RB4adcwWQjvfz~DChaaqqXN639ckRpRtS0GQ3Rc4ew3sNT87UxYDW7PfSu0gu6myb9rdWCfgvACKLmJ~-m2Hmv1V~xIei8Ks~odgOE9VeqFPE48Wreb1pJcXJ~cJXC8eXpAzh1EkcTzQGk3LHpXqWjjo2fcKJrqNLXkrVx8Qw~~A8iPKt3huMq4GfTee3N9OUtC23VSypjRBtgtRSczUExxUSuJpSx1dS~1yYoCsiQI~7gZWN19-r3RzRSlGltlrJ7Zzl~kMHgbSw4RvsyuOgowGVEx0uVMoL9SpLzzFNfV9516duv~3d~pwcVBqAa1AvAr44-UdpCMYJGJOLfGQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":10743,"name":"Coal","url":"https://www.academia.edu/Documents/in/Coal"},{"id":15836,"name":"Environmental Chemistry","url":"https://www.academia.edu/Documents/in/Environmental_Chemistry"},{"id":32712,"name":"Applied Geochemistry","url":"https://www.academia.edu/Documents/in/Applied_Geochemistry"},{"id":158165,"name":"Zinc","url":"https://www.academia.edu/Documents/in/Zinc"},{"id":526952,"name":"Fractionation","url":"https://www.academia.edu/Documents/in/Fractionation"},{"id":640682,"name":"Isotope fractionation","url":"https://www.academia.edu/Documents/in/Isotope_fractionation"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element"},{"id":1035979,"name":"Betula Pendula","url":"https://www.academia.edu/Documents/in/Betula_Pendula"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"},{"id":1957240,"name":"ENVIRONMENTAL SCIENCE AND MANAGEMENT","url":"https://www.academia.edu/Documents/in/ENVIRONMENTAL_SCIENCE_AND_MANAGEMENT"},{"id":3646326,"name":"Betula pubescens","url":"https://www.academia.edu/Documents/in/Betula_pubescens"}],"urls":[{"id":42065174,"url":"https://doi.org/10.1016/j.apgeochem.2020.104741"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267765"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology"><img alt="Research paper thumbnail of Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology" class="work-thumbnail" src="https://attachments.academia-assets.com/114677497/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology">Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology</a></div><div class="wp-workCard_item"><span>Lithos</span><span>, Aug 1, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="620097a1d6db74775ab0c1359433b2f5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677497,"asset_id":119267765,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267765"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267765"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267765; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267765]").text(description); $(".js-view-count[data-work-id=119267765]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267765; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267765']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267765, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "620097a1d6db74775ab0c1359433b2f5" } } $('.js-work-strip[data-work-id=119267765]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267765,"title":"Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Structural analysis and U-Pb geochronological study on zircons from the southern Chinese Altai (the Kalasu area, SE of the Altai city) show that the Cambro-Ordovician accretionary wedge (ca. 520-492 Ma) underwent four major geological events: 1) emplacement of Early Devonian magmas (ca. 410-400) associated with formation of a volcano-sedimentary cover, 2) major Middle Devonian (ca. 390-374 Ma) tectono-metamorphic event, 3) Late Devonian-Early Carboniferous folding without apparent metamorphism, and 4) a regional folding with localized Early Permian high-to ultrahigh-temperature reworking (ca. 300-280 Ma). The Early Devonian magmatism is characterized by emplacement of mafic rocks and granitoids in the centre of the NE-SW profile, coevally with granitoid magmatism and rhyolite volcanism in the southwest and northeast, respectively. The whole volcano-sedimentary and magmatic edifice was transposed by sub-horizontal metamorphic fabric associated with variable metamorphic degrees in different areas ranging from greenschist facies in the northeast (mu+bi±g) to amphibolite facies in the southwest (st+g±sill) and granulite facies in the centre (g+sill+kfs). This metamorphic architecture, distribution of magmatism and character of metamorphic zircon populations allow to correlate these areas with upper, middle and lower orogenic crust that developed during important vertical shortening and horizontal flow in Middle Devonian. Subsequently, the whole edifice was affected by regional NE-SW trending upright (possibly Late Devonian-Early Carboniferous) folding. Finally, Early Permian shortening produced NW-SE trending regional upright folds in the southwest and northeast and a crustal-scale vertical, tabular deformation zone in the centre. The Permian deformation is accompanied by granulite facies (kfs+cd+sill+g) metamorphism and anatexis reworking the Devonian lower orogenic crust, with extensive resetting and growth of new zircons and with intrusions of Permian granites and gabbros. This study suggests that the Early Permian event","publication_date":{"day":1,"month":8,"year":2018,"errors":{}},"publication_name":"Lithos","grobid_abstract_attachment_id":114677497},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology","translated_internal_url":"","created_at":"2024-05-17T23:06:31.947-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677497,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677497/thumbnails/1.jpg","file_name":"709629.pdf","download_url":"https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Polycyclic_Palaeozoic_evolution_of_accre.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677497/709629-libre.pdf?1716014269=\u0026response-content-disposition=attachment%3B+filename%3DPolycyclic_Palaeozoic_evolution_of_accre.pdf\u0026Expires=1733072614\u0026Signature=e2QQkBnTW6vRZoH2eJl4J6sdLLupMqd7JS1n83tofm3tu4JIcaBQfWJXUN4cyoBeHaQPzNsyt1whonXUmNpFoZ5S3zW2gzag-e3OHPjmVNReJZXwXQcQ7tb-fMbNepTVaqu8kVmU5B4LEP0W66ZbxIWUwwkQOMaF2lLa-4CszEwZ7Ew1uSU4hruEdrOraM1hMvyh7~3eklbq5Qms4DxnF0C7ls9iq-ahWQxPLesyQTW42pLzWkKOnxi6wMW3CJRXHCV5P2~xMXtrkDSEesVxxT8dlcdZTfWTjNBDC2NB8pliX5d32BhrOuMHM2x1wnbLkzwi1C~txMym1on7premMw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology","translated_slug":"","page_count":80,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677497,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677497/thumbnails/1.jpg","file_name":"709629.pdf","download_url":"https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Polycyclic_Palaeozoic_evolution_of_accre.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677497/709629-libre.pdf?1716014269=\u0026response-content-disposition=attachment%3B+filename%3DPolycyclic_Palaeozoic_evolution_of_accre.pdf\u0026Expires=1733072614\u0026Signature=e2QQkBnTW6vRZoH2eJl4J6sdLLupMqd7JS1n83tofm3tu4JIcaBQfWJXUN4cyoBeHaQPzNsyt1whonXUmNpFoZ5S3zW2gzag-e3OHPjmVNReJZXwXQcQ7tb-fMbNepTVaqu8kVmU5B4LEP0W66ZbxIWUwwkQOMaF2lLa-4CszEwZ7Ew1uSU4hruEdrOraM1hMvyh7~3eklbq5Qms4DxnF0C7ls9iq-ahWQxPLesyQTW42pLzWkKOnxi6wMW3CJRXHCV5P2~xMXtrkDSEesVxxT8dlcdZTfWTjNBDC2NB8pliX5d32BhrOuMHM2x1wnbLkzwi1C~txMym1on7premMw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":3139797,"name":"Accretionary Wedge","url":"https://www.academia.edu/Documents/in/Accretionary_Wedge"}],"urls":[{"id":42065173,"url":"http://manuscript.elsevier.com/S002449371830207X/pdf/S002449371830207X.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267764"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_"><img alt="Research paper thumbnail of Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_">Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)</a></div><div class="wp-workCard_item"><span>EGUGA</span><span>, Apr 1, 2019</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267764"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267764"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267764; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267764]").text(description); $(".js-view-count[data-work-id=119267764]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267764; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267764']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267764, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267764]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267764,"title":"Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)","translated_title":"","metadata":{"publication_date":{"day":1,"month":4,"year":2019,"errors":{}},"publication_name":"EGUGA"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_","translated_internal_url":"","created_at":"2024-05-17T23:06:31.741-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mariánské_Lázně_Complex_and_Čistá_pluton_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":1479595,"name":"Continental Margin","url":"https://www.academia.edu/Documents/in/Continental_Margin"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065172,"url":"http://ui.adsabs.harvard.edu/abs/2019EGUGA..2114335D/abstract"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267763"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia"><img alt="Research paper thumbnail of Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia" class="work-thumbnail" src="https://attachments.academia-assets.com/114677452/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia">Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia</a></div><div class="wp-workCard_item"><span>Šinžlèh uhaany akademijn mèdèè</span><span>, Dec 31, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c58301af24d773c233c0083e9fb21450" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677452,"asset_id":119267763,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267763"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267763"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267763; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267763]").text(description); $(".js-view-count[data-work-id=119267763]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267763; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267763']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267763, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c58301af24d773c233c0083e9fb21450" } } $('.js-work-strip[data-work-id=119267763]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267763,"title":"Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia","translated_title":"","metadata":{"publisher":"Mongolian Academy of Sciences","grobid_abstract":"The study area is located in the central part of Tsetserleg terrane in the southwestern margin of the Khangai-Khentey orogenic system. The paper presents new data on geochemistry and geochronology of sedimentary rocks from the Shar Khutul area, where the Tsetserleg terrane consists of Silurian-Devonian oceanic plate stratigraphic unit and Carboniferous shallow water sediment. The Upper Silurian to Middle Devonian Erdenetsogt Formation (S 3-D 2 er), which is an oceanic plate stratigraphic unit, is mainly composed of siliceous siltstone, volcanites, tuffs, quartzite, and cherts. The shallow water sediments are divided into Upper Devonian to Lower Carboniferous Tsetserleg Formation (D 3-C 1 cc) and Lower-Middle Carboniferous Dzargalant Formation (C 1-2 dz). The Tsetserleg Formation (D 3-C 1 cc) consists of only sedimentary rocks such as bluish-grey sandstones and siltstones, and Lower-Middle Carboniferous Dzargalant Formation (C 1-2 dz) is principally composed of medium-to coarse-grained, brown-greenish grey sandstones with thin-layers of dark siltstones and gravelites. The SiO 2 content of the Shar Khutul area sandstones ranges from 63.85 to 67.95 wt.% and the average content of TiO 2 is 0.72 wt.% and Al 2 O 3 content is 14.38 wt.%. The Chemical Index of Alteration (CIA) value ranges from 48.71 to 56.94 and the range of Index of compositional variations (ICV) is from 0.98 to 1.24. Moreover, the samples studied show that most of the sandstones are generally immature and were derived from weakly weathered source rocks. The ratios of Eu/Eu* (0.83), La/Sc (3.81), La/Co (5.30), and Cr/Th (13.81) indicate that the derivation of the Shar Khutul area sandstones from felsic rock sources and confirm the signatures of a felsic igneous provenance and suggest an active continental margin tectonic setting of the source area. The clastic zircons from the medium grained sandstone (Erdenetsogt formation) yield ages between 2.5 Ga and 236 Ma and the detrital zircons exhibit four peak ages at 1.","publication_date":{"day":31,"month":12,"year":2018,"errors":{}},"publication_name":"Šinžlèh uhaany akademijn mèdèè","grobid_abstract_attachment_id":114677452},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia","translated_internal_url":"","created_at":"2024-05-17T23:06:31.487-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677452,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677452/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677452/1333-libre.pdf?1716014271=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=VpwT-7Sqk8pJlYpt3cYR-FDGku7qhTiFMMzEUTMkskjYgU-bWkUElgNSxCAlllRy1LgNg48EcBeB0m~f~hf0RN5UpAQbaxh6k-Pg6kv7SizPezaDiiZPsurwOio7rgp2ljoH6O1lLGAE0gtp3MSr63VbiDiCXdSxvBxpjceTrLSfK0F0yI885qibD~UmykBUS9TVRdY8BS1na868F59NkOGwLNrkFBJYeZBp2fo~7m1O1ocgpr22SYvWQaOBl~kDFxYdfCoG~dq8GoJtx0dl5NRx18Fc4-X87jkvP0z5KXjW2pCM7Yhb2Z5BJcXYIklZ~vXI~XI9WOlXJLMmuUoQSA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia","translated_slug":"","page_count":18,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677452,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677452/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677452/1333-libre.pdf?1716014271=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=VpwT-7Sqk8pJlYpt3cYR-FDGku7qhTiFMMzEUTMkskjYgU-bWkUElgNSxCAlllRy1LgNg48EcBeB0m~f~hf0RN5UpAQbaxh6k-Pg6kv7SizPezaDiiZPsurwOio7rgp2ljoH6O1lLGAE0gtp3MSr63VbiDiCXdSxvBxpjceTrLSfK0F0yI885qibD~UmykBUS9TVRdY8BS1na868F59NkOGwLNrkFBJYeZBp2fo~7m1O1ocgpr22SYvWQaOBl~kDFxYdfCoG~dq8GoJtx0dl5NRx18Fc4-X87jkvP0z5KXjW2pCM7Yhb2Z5BJcXYIklZ~vXI~XI9WOlXJLMmuUoQSA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677453,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677453/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677453/download_file","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677453/1333-libre.pdf?1716014261=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=Crd0xw22lGrWc2H~4YT7JRPYWCpqUKBokyCkh-VuU0Yxkwh1dEu~YtEBEGfFSlZD4fQMrHmjVbNn5ddq40p24Ph-xT-pHvlyQnDO1vYDsVUhVnq0xwHjzQpxDKFj5LB5tan7jpX2-RvgtPxwv0IACrSi1Ssi7JAdKkWv2QG~orLJgDG4rL2aRlMkw5TRKw18rIhGjpNok~Pxj2MiRR0NtU-CSgnj1AmtNO58hLclh7V3I~YWLZRNKzcgelcI7iZ9wmMdTC-odmb8RkOQY8gSq-TSOiAAP-tuqUOMecQFIqHrLxOMexa9ca0Os0IeTLVmYBTf6KfZTzCh-M6TG94mpQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76409,"name":"Tectonic Setting","url":"https://www.academia.edu/Documents/in/Tectonic_Setting"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":479964,"name":"Siltstone","url":"https://www.academia.edu/Documents/in/Siltstone"},{"id":976620,"name":"Sedimentary Rocks","url":"https://www.academia.edu/Documents/in/Sedimentary_Rocks"},{"id":1567560,"name":"Sedimentary Rock","url":"https://www.academia.edu/Documents/in/Sedimentary_Rock"}],"urls":[{"id":42065171,"url":"https://www.mongoliajol.info/index.php/PMAS/article/download/1045/1333"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267762"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery"><img alt="Research paper thumbnail of Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery">Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery</a></div><div class="wp-workCard_item"><span>Geoscience frontiers</span><span>, Mar 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267762"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267762"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267762; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267762]").text(description); $(".js-view-count[data-work-id=119267762]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267762; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267762']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267762, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267762]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267762,"title":"Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":3,"year":2023,"errors":{}},"publication_name":"Geoscience frontiers"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery","translated_internal_url":"","created_at":"2024-05-17T23:06:31.247-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":135982,"name":"Rodinia","url":"https://www.academia.edu/Documents/in/Rodinia"},{"id":135985,"name":"Orogeny","url":"https://www.academia.edu/Documents/in/Orogeny"},{"id":166969,"name":"Gneiss","url":"https://www.academia.edu/Documents/in/Gneiss"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":319883,"name":"Supercontinent","url":"https://www.academia.edu/Documents/in/Supercontinent"},{"id":1590367,"name":"Monazite","url":"https://www.academia.edu/Documents/in/Monazite"},{"id":1865674,"name":"Schist","url":"https://www.academia.edu/Documents/in/Schist"},{"id":3160824,"name":"Sillimanite","url":"https://www.academia.edu/Documents/in/Sillimanite"},{"id":3265172,"name":"kyanite","url":"https://www.academia.edu/Documents/in/kyanite"}],"urls":[{"id":42065170,"url":"https://doi.org/10.1016/j.gsf.2022.101520"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267761"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_"><img alt="Research paper thumbnail of Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_">Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)</a></div><div class="wp-workCard_item"><span>Geoscience frontiers</span><span>, May 1, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267761"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267761"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267761; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267761]").text(description); $(".js-view-count[data-work-id=119267761]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267761; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267761']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267761, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267761]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267761,"title":"Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":5,"year":2022,"errors":{}},"publication_name":"Geoscience frontiers"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_","translated_internal_url":"","created_at":"2024-05-17T23:06:30.995-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065169,"url":"https://doi.org/10.1016/j.gsf.2022.101374"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267760"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage"><img alt="Research paper thumbnail of From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage">From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage</a></div><div class="wp-workCard_item"><span>Gondwana Research</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267760"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267760"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267760; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267760]").text(description); $(".js-view-count[data-work-id=119267760]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267760; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267760']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267760, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267760]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267760,"title":"From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_name":"Gondwana Research"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage","translated_internal_url":"","created_at":"2024-05-17T23:06:30.750-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":191873,"name":"Magmatism","url":"https://www.academia.edu/Documents/in/Magmatism"},{"id":319872,"name":"Continental-arc","url":"https://www.academia.edu/Documents/in/Continental-arc"},{"id":421956,"name":"Continental Crust","url":"https://www.academia.edu/Documents/in/Continental_Crust"},{"id":3382937,"name":"felsic","url":"https://www.academia.edu/Documents/in/felsic"}],"urls":[{"id":42065168,"url":"https://api.elsevier.com/content/article/PII:S1342937X23001314?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267759"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif"><img alt="Research paper thumbnail of U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif" class="work-thumbnail" src="https://attachments.academia-assets.com/114677495/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif">U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif</a></div><div class="wp-workCard_item"><span>Journal of African Earth Sciences</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b8e24fa6e0198451f743a7369b5fab9b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677495,"asset_id":119267759,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267759"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267759"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267759; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267759]").text(description); $(".js-view-count[data-work-id=119267759]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267759; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267759']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267759, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b8e24fa6e0198451f743a7369b5fab9b" } } $('.js-work-strip[data-work-id=119267759]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267759,"title":"U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"HAL is a multidisciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L'archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d'enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.","publication_name":"Journal of African Earth Sciences","grobid_abstract_attachment_id":114677495},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif","translated_internal_url":"","created_at":"2024-05-17T23:06:30.450-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677495,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677495/thumbnails/1.jpg","file_name":"20220502_Rehamna_Revised_20manuscript_HAL.pdf","download_url":"https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_detrital_zircon_geochronology_and_s.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677495/20220502_Rehamna_Revised_20manuscript_HAL-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_detrital_zircon_geochronology_and_s.pdf\u0026Expires=1733072614\u0026Signature=cGOp42YeOnwtcdgn5KveKfmiJZflp2AGeX3ykub-UhS0cdg7PH9fsqUfHW4JA8qTgtiF0~~PF1pq5fEZMLL3c0PHGQpsN2XmWLbVRXL~xkr2vmYQbHDZA8eGh9j2p6Awo~ZVs2gKm5kjYXCVa0LrNed9T-vRp19xr97WyKx38ETFR8Br1zfdmjjs30Kq0gsOHNGnTA4ec6idUawMEmcEv4fMC8eCpqG964NW-8nXCV4kHTrWqYp02dbaGqKKx0APLzffexQmuQpAQxv4A~KXrLQnqhSvgUHgUGcH2LkgaeNEUFhEMaUwuQwJYQRZoTAK6uKIGIQwC~xeFfbQyi5HZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif","translated_slug":"","page_count":39,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677495,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677495/thumbnails/1.jpg","file_name":"20220502_Rehamna_Revised_20manuscript_HAL.pdf","download_url":"https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_detrital_zircon_geochronology_and_s.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677495/20220502_Rehamna_Revised_20manuscript_HAL-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_detrital_zircon_geochronology_and_s.pdf\u0026Expires=1733072614\u0026Signature=cGOp42YeOnwtcdgn5KveKfmiJZflp2AGeX3ykub-UhS0cdg7PH9fsqUfHW4JA8qTgtiF0~~PF1pq5fEZMLL3c0PHGQpsN2XmWLbVRXL~xkr2vmYQbHDZA8eGh9j2p6Awo~ZVs2gKm5kjYXCVa0LrNed9T-vRp19xr97WyKx38ETFR8Br1zfdmjjs30Kq0gsOHNGnTA4ec6idUawMEmcEv4fMC8eCpqG964NW-8nXCV4kHTrWqYp02dbaGqKKx0APLzffexQmuQpAQxv4A~KXrLQnqhSvgUHgUGcH2LkgaeNEUFhEMaUwuQwJYQRZoTAK6uKIGIQwC~xeFfbQyi5HZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":1305086,"name":"Basement","url":"https://www.academia.edu/Documents/in/Basement"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065167,"url":"https://api.elsevier.com/content/article/PII:S1464343X22001625?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267758"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone"><img alt="Research paper thumbnail of Paleozoic geodynamics and architecture of the Mongolian Altai Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/114677494/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone">Paleozoic geodynamics and architecture of the Mongolian Altai Zone</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ad25b9318dc060e6aba76cdb70afc150" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677494,"asset_id":119267758,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267758"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267758"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267758; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267758]").text(description); $(".js-view-count[data-work-id=119267758]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267758; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267758']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267758, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ad25b9318dc060e6aba76cdb70afc150" } } $('.js-work-strip[data-work-id=119267758]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267758,"title":"Paleozoic geodynamics and architecture of the Mongolian Altai Zone","translated_title":"","metadata":{"publisher":"Copernicus GmbH","publication_date":{"day":null,"month":null,"year":2022,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone","translated_internal_url":"","created_at":"2024-05-17T23:06:30.298-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677494,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677494/thumbnails/1.jpg","file_name":"723920.pdf","download_url":"https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_geodynamics_and_architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677494/723920-libre.pdf?1716014243=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_geodynamics_and_architecture_o.pdf\u0026Expires=1733072614\u0026Signature=HBPEin89jMmIsJn83Jj6-92ZYYE0NArkVVdJtg9D-OY8x74Oar~hfQa~9hXSV5XmEhw3X5TofecJ89lOafo6ydgaOlSze89M-BLNUazGqqJqAsjLrZjeyo-KkV-g7JOSDCRmXAs9JCFpj7Ps1kb5KJzsT0afzAttzBDvzYdzOrIWqvm1vzNGN1-ktiHt445Xhh6rhb3TKaYIFtdAjsQyvaqc7WVrdjv8YZoEEyxmH1J7zai4MNja7BvjrbzZ4IoWlmfj9x~xjhuOF2IgXBOySVE6-S7cyT6dGDrAXQI0i6VEg6P8-kQPgB3TwoCEVSj-7YnEY4Cc4vHGgT9nmKzPOg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone","translated_slug":"","page_count":2,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677494,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677494/thumbnails/1.jpg","file_name":"723920.pdf","download_url":"https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_geodynamics_and_architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677494/723920-libre.pdf?1716014243=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_geodynamics_and_architecture_o.pdf\u0026Expires=1733072614\u0026Signature=HBPEin89jMmIsJn83Jj6-92ZYYE0NArkVVdJtg9D-OY8x74Oar~hfQa~9hXSV5XmEhw3X5TofecJ89lOafo6ydgaOlSze89M-BLNUazGqqJqAsjLrZjeyo-KkV-g7JOSDCRmXAs9JCFpj7Ps1kb5KJzsT0afzAttzBDvzYdzOrIWqvm1vzNGN1-ktiHt445Xhh6rhb3TKaYIFtdAjsQyvaqc7WVrdjv8YZoEEyxmH1J7zai4MNja7BvjrbzZ4IoWlmfj9x~xjhuOF2IgXBOySVE6-S7cyT6dGDrAXQI0i6VEg6P8-kQPgB3TwoCEVSj-7YnEY4Cc4vHGgT9nmKzPOg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":78102,"name":"Archean","url":"https://www.academia.edu/Documents/in/Archean"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":469741,"name":"Craton","url":"https://www.academia.edu/Documents/in/Craton"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267757"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution"><img alt="Research paper thumbnail of Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution">Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution</a></div><div class="wp-workCard_item"><span>EGUGA</span><span>, Apr 1, 2019</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267757"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267757"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267757; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267757]").text(description); $(".js-view-count[data-work-id=119267757]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267757; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267757']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267757, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267757]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267757,"title":"Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution","translated_title":"","metadata":{"publication_date":{"day":1,"month":4,"year":2019,"errors":{}},"publication_name":"EGUGA"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution","translated_internal_url":"","created_at":"2024-05-17T23:06:29.756-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_Góry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065166,"url":"http://ui.adsabs.harvard.edu/abs/2019EGUGA..2113714T/abstract"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267756"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain"><img alt="Research paper thumbnail of Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain" class="work-thumbnail" src="https://attachments.academia-assets.com/114677492/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain">Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain</a></div><div class="wp-workCard_item"><span>Precambrian Research</span><span>, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3ec7dcd168a180c7412df210cb76ca3f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677492,"asset_id":119267756,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267756"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267756"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267756; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267756]").text(description); $(".js-view-count[data-work-id=119267756]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267756; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267756']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267756, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "3ec7dcd168a180c7412df210cb76ca3f" } } $('.js-work-strip[data-work-id=119267756]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267756,"title":"Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"In this study, U-Pb ages and Hf isotopic composition of detrital zircons from the Precambrian metasedimentary autochthon of the Brunovistulian Domain in the eastern Bohemian Massif were investigated to understand the pre-collisional evolution of the eastern periphery of the European Variscan belt. Detrital zircons of the Tonian sequences have mostly Paleoproterozoic to Neoproterozoic ages (c. 2.1-0.9 Ga) and are interpreted as detritus derived from the basement of either Baltica or Amazonia. The mostly positive ε Hf(t) values (-4 to +16) indicate a juvenile nature of their magma sources with minor older crustal components. In contrast, the Ediacaran sequences contain dominantly Neoproterozoic zircons (c. 600 Ma) and only rare Paleo-and Mesoproterozoic ages indicate that they were sourced from the adjacent Neoproterozoic magmatic arc with very limited input of recycled cratonic detritus. The large spread of ε Hf(t) values (-15 to +13) of the Neoproterozoic zircons suggests significant mixing of mantle-derived magmas with mature crustal material, typical of large continental magmatic arc systems. The zircon age patterns of the Ediacaran sequences, characterized by a dominance of the late Neoproterozoic zircons and limited Mesoproterozoic zircons, are nearly identical to those from the Teplá-Barrandian Unit and Moldanubian Zone, pointing to their similar sources. We consider such age populations as a record of sources actually exposed at the time of deposition, rather than the real provenance signature of the continental basement. The change in detrital zircon U-Pb age and Hf record of the Brunovistulian Domain took place between the early and late Neoproteorozoic, and probably reflects the plate-tectonic reconfiguration from the Rodinia formation/break-up to the evolution of the Gondwana or Baltica active margins. Our data challenge the main arguments for an existence of the Rheic oceanic suture between the Brunovistulian Domain and-Moldanubian Zone and allow for an alternative pre-collisional model of the Bohemian Massif as a single Neoproterozoic crustal domain.","publication_date":{"day":null,"month":null,"year":2022,"errors":{}},"publication_name":"Precambrian Research","grobid_abstract_attachment_id":114677492},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain","translated_internal_url":"","created_at":"2024-05-17T23:06:29.547-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677492,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677492/thumbnails/1.jpg","file_name":"article.pdf","download_url":"https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Pre_collisional_crustal_evolution_of_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677492/article-libre.pdf?1716014584=\u0026response-content-disposition=attachment%3B+filename%3DPre_collisional_crustal_evolution_of_the.pdf\u0026Expires=1733072614\u0026Signature=c3VvVRz9MptoHuD8oUXTpoUq8aqSWhsvC3RY1Ar5CpuXakLpPhEF2JiJRQ3293TavvUAF00nU4Im~TaXFzZUjydceT40W3s2FbCPdbJnvmf72YRyTPNAciX3zcLIaV1hoIvrjrvghZqo1Zbtl6CnBHPiZ5tyNeaolf5JH0tP8QCpT89353WAPLMG0gsL0ZpoI-O-Xh9MYsteojTzihyOWHgHaDtxGO~RiAimXN8q70n5TP4bUCwOTSOf-MISxYj2izvidr~mTtpFtWGIo757LLT~2QF1aX5fasQ66RQAHB~qfezZmkjulc70dYZqTYFQHr0BRJUOHK56LyIButVNLg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain","translated_slug":"","page_count":64,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677492,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677492/thumbnails/1.jpg","file_name":"article.pdf","download_url":"https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Pre_collisional_crustal_evolution_of_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677492/article-libre.pdf?1716014584=\u0026response-content-disposition=attachment%3B+filename%3DPre_collisional_crustal_evolution_of_the.pdf\u0026Expires=1733072614\u0026Signature=c3VvVRz9MptoHuD8oUXTpoUq8aqSWhsvC3RY1Ar5CpuXakLpPhEF2JiJRQ3293TavvUAF00nU4Im~TaXFzZUjydceT40W3s2FbCPdbJnvmf72YRyTPNAciX3zcLIaV1hoIvrjrvghZqo1Zbtl6CnBHPiZ5tyNeaolf5JH0tP8QCpT89353WAPLMG0gsL0ZpoI-O-Xh9MYsteojTzihyOWHgHaDtxGO~RiAimXN8q70n5TP4bUCwOTSOf-MISxYj2izvidr~mTtpFtWGIo757LLT~2QF1aX5fasQ66RQAHB~qfezZmkjulc70dYZqTYFQHr0BRJUOHK56LyIButVNLg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":579156,"name":"Detritus","url":"https://www.academia.edu/Documents/in/Detritus"},{"id":1305086,"name":"Basement","url":"https://www.academia.edu/Documents/in/Basement"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065165,"url":"https://api.elsevier.com/content/article/PII:S030192682200050X?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267755"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif"><img alt="Research paper thumbnail of Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif">Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif</a></div><div class="wp-workCard_item"><span>Journal of the Geological Society</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the interna...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267755"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267755"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267755; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267755]").text(description); $(".js-view-count[data-work-id=119267755]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267755; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267755']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267755, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267755]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267755,"title":"Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif","translated_title":"","metadata":{"abstract":"The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"Journal of the Geological Society"},"translated_abstract":"The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...","internal_url":"https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif","translated_internal_url":"","created_at":"2024-05-17T23:06:29.345-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065164,"url":"https://syndication.highwire.org/content/doi/10.1144/jgs2020-176"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div><div class="profile--tab_content_container js-tab-pane tab-pane" data-section-id="461848" id="papers"><div class="js-work-strip profile--work_container" data-work-id="119267774"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge"><img alt="Research paper thumbnail of Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge" class="work-thumbnail" src="https://attachments.academia-assets.com/114677499/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge">Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge</a></div><div class="wp-workCard_item"><span>Journal of Structural Geology</span><span>, 2017</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="e65a6d76dfbe9de31751fdf6322750d8" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677499,"asset_id":119267774,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267774"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267774"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267774; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267774]").text(description); $(".js-view-count[data-work-id=119267774]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267774; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267774']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267774, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "e65a6d76dfbe9de31751fdf6322750d8" } } $('.js-work-strip[data-work-id=119267774]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267774,"title":"Magnetic fabric transposition in folded granite sills in Variscan orogenic wedge","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"New approach involving evaluation of anisotropy of magnetic susceptibility (AMS) data in stereoplots and Jelinek's P j-T space, Vollmer's eigenvalue and microstructural analyses is proposed to discriminate between homogeneous and superposed deformation in granites. This method is used to decipher the internal AMS fabric and microstructural evolution of a folded array of granitic sills. The studied major sill shows a fabric and microstructural zonality marked by submagmatic and high-temperature Type I planar-linear fabric developed at sill margins, and the transpositional Type II subsolidus fabrics that formed at high to medium temperatures deformation in the sill core. While Type I fabric is associated with dip slip magnetic lineations, Type II subsolidus fabrics are marked by subhorizontal","publication_date":{"day":null,"month":null,"year":2017,"errors":{}},"publication_name":"Journal of Structural Geology","grobid_abstract_attachment_id":114677499},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267774/Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge","translated_internal_url":"","created_at":"2024-05-17T23:06:34.160-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677499,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677499/thumbnails/1.jpg","file_name":"j.jsg.2016.11.00720240518-1-obyqzb.pdf","download_url":"https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Magnetic_fabric_transposition_in_folded.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677499/j.jsg.2016.11.00720240518-1-obyqzb-libre.pdf?1716019973=\u0026response-content-disposition=attachment%3B+filename%3DMagnetic_fabric_transposition_in_folded.pdf\u0026Expires=1733072613\u0026Signature=AWPWWapcuGjyhBpUI1MNX674TuU0cOQe~x6d3kCxFGZcdzjfSlH3s1t2VMlemnSk7FjkJEpan0KMUAaXwK5rBRHkj6UvmGeJfAVDDI~uHr82od~RPIuOvQ7VOM2p9m-y7TWyv4Xo9iBgLsJ89288X6MxI3YlG0nMiCAy4CfEaygFMmH2~NQC-FI6ZMgKHG-Mq7D3NOj0FUHFjd800yGqUoEds7lZVcPpC2m~BMaX7VST-LABij0RMkdEX4NJMy4x6QZqgBbIDH2qbbLj6D0DtX58uZjeisQxy2Tpow2X5SHqtFY0-6TOfhZFVuKOXqrmhWsOrDaYK51L9Rzg0MgABg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Magnetic_fabric_transposition_in_folded_granite_sills_in_Variscan_orogenic_wedge","translated_slug":"","page_count":57,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677499,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677499/thumbnails/1.jpg","file_name":"j.jsg.2016.11.00720240518-1-obyqzb.pdf","download_url":"https://www.academia.edu/attachments/114677499/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Magnetic_fabric_transposition_in_folded.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677499/j.jsg.2016.11.00720240518-1-obyqzb-libre.pdf?1716019973=\u0026response-content-disposition=attachment%3B+filename%3DMagnetic_fabric_transposition_in_folded.pdf\u0026Expires=1733072613\u0026Signature=AWPWWapcuGjyhBpUI1MNX674TuU0cOQe~x6d3kCxFGZcdzjfSlH3s1t2VMlemnSk7FjkJEpan0KMUAaXwK5rBRHkj6UvmGeJfAVDDI~uHr82od~RPIuOvQ7VOM2p9m-y7TWyv4Xo9iBgLsJ89288X6MxI3YlG0nMiCAy4CfEaygFMmH2~NQC-FI6ZMgKHG-Mq7D3NOj0FUHFjd800yGqUoEds7lZVcPpC2m~BMaX7VST-LABij0RMkdEX4NJMy4x6QZqgBbIDH2qbbLj6D0DtX58uZjeisQxy2Tpow2X5SHqtFY0-6TOfhZFVuKOXqrmhWsOrDaYK51L9Rzg0MgABg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":1419,"name":"Structural Geology","url":"https://www.academia.edu/Documents/in/Structural_Geology"},{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology"},{"id":197590,"name":"Sill","url":"https://www.academia.edu/Documents/in/Sill"}],"urls":[{"id":42065182,"url":"https://doi.org/10.1016/j.jsg.2016.11.007"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267773"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160"><img alt="Research paper thumbnail of Hybridization of magmas by break down of partially molten granitic rock and its assimilation&amp;#160" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160">Hybridization of magmas by break down of partially molten granitic rock and its assimilation&amp;#160</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;amp;lt;p&amp;amp;amp;gt;During orogenic processes continental crust experiences signific...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">&amp;amp;amp;lt;p&amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg&amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg&amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg&amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg&amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330&amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310&amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg&amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.&amp;amp;amp;lt;/p&amp;amp;amp;gt;</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267773"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267773"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267773; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267773]").text(description); $(".js-view-count[data-work-id=119267773]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267773; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267773']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267773, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267773]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267773,"title":"Hybridization of magmas by break down of partially molten granitic rock and its assimilation\u0026amp;#160","translated_title":"","metadata":{"abstract":"\u0026amp;amp;amp;lt;p\u0026amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg\u0026amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg\u0026amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg\u0026amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg\u0026amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330\u0026amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310\u0026amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg\u0026amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.\u0026amp;amp;amp;lt;/p\u0026amp;amp;amp;gt;","publication_date":{"day":27,"month":3,"year":2022,"errors":{}}},"translated_abstract":"\u0026amp;amp;amp;lt;p\u0026amp;amp;amp;gt;During orogenic processes continental crust experiences significant partial melting. Repeated thermal pulses or fluctuation in fluid content can even cause multiple anatectic events that result in complex intrusion suits. The Vosges Mountains (NE France) reveal two chronologically and geochemically distinct tectono-magmatic events. An early major pulse of Mg\u0026amp;amp;amp;amp;#8210;K magmatism was followed ten millions years later by development of a magma-rich detachment zone and intrusion of Central Vosges Granite forming a felsic MASH zone. This MASH zone is characterized by the production of a large quantity of anatectic melts that interacted with the older Mg\u0026amp;amp;amp;amp;#8210;K granites and surrounding granulites and metasedimentary rocks. We aim to understand how such hybridization processes impact on the crustal rocks rheology, deformation as well as its geochemistry and geochronology. Three different granite varieties were distinguished: (i) the older Mg\u0026amp;amp;amp;amp;#8210;K granite end-member that is coarse-grained with a high proportion of feldspar phenocrysts, zircon U-Pb ages of 340 Ma and specific geochemical signature; (ii) Medium-grained type has a smaller amount of phenocrysts and shows advanced brecciation where fine-grained Pl+Kfs+Qtz form discontinuous corridors to an interconnected network surrounding fractured phenocrysts. Its geochemical signature suggests that this represents a mixing of Mg\u0026amp;amp;amp;amp;#8722;K and Central Vosges granites, as confirmed by the presence of both inherited (340 Ma) and younger (330\u0026amp;amp;amp;amp;#8210;310 Ma) zircon domains; (iii) Isotropic medium-grained granite that shows geochemical signature typical for the Central Vosges Granite in which younger zircon domains (310\u0026amp;amp;amp;amp;#8210;320 Ma) dominate over inherited xenocrysts (340 Ma). These three granite varieties represent different stages of magma hybridization by the break up of the older Mg\u0026amp;amp;amp;amp;#8210;K granite by the younger Central Vosges Granite magmas. The interaction between new melt and previously crystallized granitoids results in variety of granite textures, fabrics, chemical compositions, isotopic signatures and deformational behavior. In summary, the resulting signature is result of interplay of melt transfer and interaction in the MASH zone.\u0026amp;amp;amp;lt;/p\u0026amp;amp;amp;gt;","internal_url":"https://www.academia.edu/119267773/Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160","translated_internal_url":"","created_at":"2024-05-17T23:06:33.940-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Hybridization_of_magmas_by_break_down_of_partially_molten_granitic_rock_and_its_assimilation_and_amp_160","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":197592,"name":"Magma","url":"https://www.academia.edu/Documents/in/Magma"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":415323,"name":"Phenocryst","url":"https://www.academia.edu/Documents/in/Phenocryst"},{"id":2601101,"name":"Granulite","url":"https://www.academia.edu/Documents/in/Granulite"},{"id":3382937,"name":"felsic","url":"https://www.academia.edu/Documents/in/felsic"}],"urls":[{"id":42065181,"url":"https://doi.org/10.5194/egusphere-egu22-2449"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267772"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation"><img alt="Research paper thumbnail of LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation">LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation</a></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">&amp;amp;lt;p&amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observati...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">&amp;amp;lt;p&amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation&amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 &amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600&amp;amp;amp;#8211;625 &amp;amp;amp;#176;C and 1.6&amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 &amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. &amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian&amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.&amp;amp;lt;/p&amp;amp;gt;</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267772"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267772"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267772; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267772]").text(description); $(".js-view-count[data-work-id=119267772]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267772; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267772']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267772, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267772]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267772,"title":"LP-HT metamorphism in the Jebilet Massif (Moroccan variscan belt): from Paleothetys opening to Pangea formation","translated_title":"","metadata":{"abstract":"\u0026amp;amp;lt;p\u0026amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation\u0026amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 \u0026amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600\u0026amp;amp;amp;#8211;625 \u0026amp;amp;amp;#176;C and 1.6\u0026amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 \u0026amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. \u0026amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian\u0026amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.\u0026amp;amp;lt;/p\u0026amp;amp;gt;","publication_date":{"day":28,"month":3,"year":2022,"errors":{}}},"translated_abstract":"\u0026amp;amp;lt;p\u0026amp;amp;gt;In the westernmost part of the Variscan belt, petro-structural observations, mineral equilibria modelling and U-Pb age determination were carried in the Jebilet massif (Morocco), in order to precise the deformation\u0026amp;amp;amp;#8211;metamorphism of NW Africa during Late Paleozoic Variscan events. A first episode corresponds to the emplacement of the main Oulad Ouaslam intrusion at 335.2 \u0026amp;amp;amp;#177; 0.8 Ma (U-Pb LA-ICP MS on zircon) within a Visean intracontinental basin. A second episode correspond S to SE convergence resulting into nappe stacking and upright folding in the supracrustal level together with the progressive development of a sub-horizontal metamorphic foliation around the pre-heated pelitic country rocks of the intrusion up to the sillimanite zone. Crd-And growth during this event in metapelite indicate indicating heating and increase of pressure up to 600\u0026amp;amp;amp;#8211;625 \u0026amp;amp;amp;#176;C and 1.6\u0026amp;amp;amp;#8211;2.0 kbar. The timing of this sequence in metapelite is constrained by the U-Pb monazite age of 323.4 \u0026amp;amp;amp;#177; 3.6 Ma, interpreted as minimum age of metamorphic peak conditions, ca. \u0026amp;amp;lt;15 Ma younger than the emplacement of the intrusion. This very moderate thickening is followed by WNW convergence, sub-orthogonal to the first one, affecting all the previous structures and continuing probably up to the Cisuralian, similar to neighboring massifs. The first episode coincides with emplacement of magma within Visean intracontinental basins at the western tip of the ongoing opening Palaeo-Tethys Ocean, whereas the monazite dating document for the first time the precocious onset, during Late Serpukhovian\u0026amp;amp;amp;#8211;Early Bashkirian of the convergence in the NW African Variscan segment.\u0026amp;amp;lt;/p\u0026amp;amp;gt;","internal_url":"https://www.academia.edu/119267772/LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation","translated_internal_url":"","created_at":"2024-05-17T23:06:33.735-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"LP_HT_metamorphism_in_the_Jebilet_Massif_Moroccan_variscan_belt_from_Paleothetys_opening_to_Pangea_formation","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":1590367,"name":"Monazite","url":"https://www.academia.edu/Documents/in/Monazite"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065180,"url":"https://doi.org/10.5194/egusphere-egu22-9227"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267771"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_"><img alt="Research paper thumbnail of Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_">Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267771"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267771"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267771; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267771]").text(description); $(".js-view-count[data-work-id=119267771]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267771; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267771']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267771, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267771]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267771,"title":"Potassic Granulites from the Blansky Les Massif (Moldanubian Zone, Bohemian Massif)","translated_title":"","metadata":{"publication_date":{"day":null,"month":null,"year":2007,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267771/Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_","translated_internal_url":"","created_at":"2024-05-17T23:06:33.535-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Potassic_Granulites_from_the_Blansky_Les_Massif_Moldanubian_Zone_Bohemian_Massif_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":2601101,"name":"Granulite","url":"https://www.academia.edu/Documents/in/Granulite"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065179,"url":"https://uni-salzburg.elsevierpure.com/en/publications/potassic-granulites-from-the-blansky-les-massif-moldanubian-zone-"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267770"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_"><img alt="Research paper thumbnail of Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_">Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]</a></div><div class="wp-workCard_item"><span>Gondwana Research</span><span>, Dec 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267770"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267770"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267770; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267770]").text(description); $(".js-view-count[data-work-id=119267770]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267770; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267770']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267770, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267770]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267770,"title":"Corrigendum to “U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications” [Gondwana Res. 117 (2023) 274–294]","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":12,"year":2023,"errors":{}},"publication_name":"Gondwana Research"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267770/Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_","translated_internal_url":"","created_at":"2024-05-17T23:06:33.265-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Corrigendum_to_U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications_Gondwana_Res_117_2023_274_294_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"}],"urls":[{"id":42065178,"url":"https://doi.org/10.1016/j.gr.2023.06.016"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267769"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa"><img alt="Research paper thumbnail of U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa">U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267769"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267769"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267769; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267769]").text(description); $(".js-view-count[data-work-id=119267769]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267769; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267769']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267769, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267769]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267769,"title":"U-Pb geochronology of granitoids from northern Morocco: a two-step tale for the evolution of the Variscan domain in NW Africa","translated_title":"","metadata":{"publication_date":{"day":28,"month":3,"year":2022,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267769/U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa","translated_internal_url":"","created_at":"2024-05-17T23:06:32.850-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"U_Pb_geochronology_of_granitoids_from_northern_Morocco_a_two_step_tale_for_the_evolution_of_the_Variscan_domain_in_NW_Africa","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065177,"url":"https://doi.org/10.5194/egusphere-egu22-12505"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267768"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone"><img alt="Research paper thumbnail of Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/114677454/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone">Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone</a></div><div class="wp-workCard_item"><span>Tectonics</span><span>, Aug 1, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c59b21ed364b99116d1b5f1c67e17b56" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677454,"asset_id":119267768,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267768"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267768"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267768; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267768]").text(description); $(".js-view-count[data-work-id=119267768]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267768; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267768']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267768, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c59b21ed364b99116d1b5f1c67e17b56" } } $('.js-work-strip[data-work-id=119267768]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267768,"title":"Paleozoic Geodynamics and Architecture of the Southern Part of the Mongolian Altai Zone","translated_title":"","metadata":{"publisher":"Wiley-Blackwell","ai_title_tag":"Paleozoic Geodynamics of Mongolian Altai Accretionary Wedge","grobid_abstract":"An important component of all accretionary systems is the up to 20 km-thick volcanic-sedimentary wedge built above the subducting plate, in front of a magmatic arc and upper plate continent (Cawood et al., 2009). This wedge, often several thousand kilometers long and hundreds of kilometers wide, is accreted during the ca. 100 Ma lifetime of oceanic spreading and subduction (Kusky et al., 2013). The main wedge feature is the so-called ocean plate stratigraphy with the oldest pillow lavas, bedded cherts, deep marine siliceous fine-grained sediments, and the youngest turbidites derived from a continent and magmatic arc. This sequence is often imbricated together with seamount volcanic products, and is later intruded by an oceanward migrating magmatic arc due to a continuous rollback of a subducting plate. The entire process produces a typical lithological association of Pacific-type active margins (Collins, 2002). Based on this, a classical Japan Islands-type scenario was proposed for the volcano-sedimentary accretionary prism of the Mongolian Altai Zone, one of the main constituents of the Mongolian Collage System (Long et al., 2007; Xiao, Kusky, et al., 2015). The Mongolian Altai Zone consists mainly of thick late Cambrian and Ordovician sedimentary packages covered by Silurian and Devonian volcano-clastic sequences (","publication_date":{"day":1,"month":8,"year":2022,"errors":{}},"publication_name":"Tectonics","grobid_abstract_attachment_id":114677454},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267768/Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone","translated_internal_url":"","created_at":"2024-05-17T23:06:32.653-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677454,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677454/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677454/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=ASNhunF-wCYXT-4a79lxGZw7lRkQfpog0aRlFK5P2F5k7YEQfGItOTlqseZMGVjPiH58py2ABxE-1r41xHwO6dmldZrl8p8ZDbaGfrtK9hkC96fHTWbczBLylwOMgCn8Q0EIzrwQqGJbe1k6JQL6dPSwmES1-RCpC8kKnJAYd~kDVosHvJ7AdgfuoLFfqCda8IoVr7thQgF~whp2KZUdDI8QaOrmrFczD15lK8VNEi-DLTERJz7e4Mpu4vAwdPZs4pwkZRi0nIVU1PBG8NK7DEmlvqQ2ID3Q9n-zhlMnnm4NKLKQGi5ecrcOIOykuMEXEx~Z2mQ4GFQZZeWeasATgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Paleozoic_Geodynamics_and_Architecture_of_the_Southern_Part_of_the_Mongolian_Altai_Zone","translated_slug":"","page_count":36,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677454,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677454/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677454/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677454/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=ASNhunF-wCYXT-4a79lxGZw7lRkQfpog0aRlFK5P2F5k7YEQfGItOTlqseZMGVjPiH58py2ABxE-1r41xHwO6dmldZrl8p8ZDbaGfrtK9hkC96fHTWbczBLylwOMgCn8Q0EIzrwQqGJbe1k6JQL6dPSwmES1-RCpC8kKnJAYd~kDVosHvJ7AdgfuoLFfqCda8IoVr7thQgF~whp2KZUdDI8QaOrmrFczD15lK8VNEi-DLTERJz7e4Mpu4vAwdPZs4pwkZRi0nIVU1PBG8NK7DEmlvqQ2ID3Q9n-zhlMnnm4NKLKQGi5ecrcOIOykuMEXEx~Z2mQ4GFQZZeWeasATgw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677455,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677455/thumbnails/1.jpg","file_name":"724585.pdf","download_url":"https://www.academia.edu/attachments/114677455/download_file","bulk_download_file_name":"Paleozoic_Geodynamics_and_Architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677455/724585-libre.pdf?1716014278=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_Geodynamics_and_Architecture_o.pdf\u0026Expires=1733072613\u0026Signature=SNK2HbP~fMDtoy29Wk8u37P88mq38CtEtfp-WJZVz8vA~q2lc7doN3644TQGXOZOMjCbBjNlQj9csaSzYoeRoMvYvVLCL8qlBs1BXpbp-xoyO0zNtDdjDUMwCi915pZDqeUzBusmngRUvz1OgZ~GY3d5EeUmskItq3672mO-a~BehatOLzM5xs0ytXBWxDSaFdI4IgA3B3XPh0nTTJK45ag4vq8LhqqR5DRxz1ogkOP1QIcsrQMWOdhc8TayNTHKjKUZ4iYiv~jGRf2Uz9ph41de3CeUsQahmvfHrgfWKXRnxamQsP7hdR0zxXcUybUHwSrWTRcPibQKzP60Ju~ngQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":101506,"name":"Permian","url":"https://www.academia.edu/Documents/in/Permian"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"}],"urls":[{"id":42065176,"url":"http://diposit.ub.edu/dspace/bitstream/2445/188707/1/724585.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267767"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications"><img alt="Research paper thumbnail of U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications" class="work-thumbnail" src="https://attachments.academia-assets.com/114677457/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications">U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications</a></div><div class="wp-workCard_item"><span>Gondwana Research</span><span>, May 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c607c5d2009dada2bf684a89c0bbb8a1" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677457,"asset_id":119267767,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267767"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267767"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267767; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267767]").text(description); $(".js-view-count[data-work-id=119267767]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267767; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267767']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267767, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c607c5d2009dada2bf684a89c0bbb8a1" } } $('.js-work-strip[data-work-id=119267767]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267767,"title":"U–Pb geochronology of Variscan granitoids from the Moroccan Meseta (Northwest Africa): Tectonic implications","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"This is a PDF file of an article that has undergone enhancements after acceptance, such as the addition of a cover page and metadata, and formatting for readability, but it is not yet the definitive version of record. This version will undergo additional copyediting, typesetting and review before it is published in its final form, but we are providing this version to give early visibility of the article. Please note that, during the production process, errors may be discovered which could affect the content, and all legal disclaimers that apply to the journal pertain.","publication_date":{"day":1,"month":5,"year":2023,"errors":{}},"publication_name":"Gondwana Research","grobid_abstract_attachment_id":114677457},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267767/U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications","translated_internal_url":"","created_at":"2024-05-17T23:06:32.427-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677457,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677457/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677457/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=E~y7Ty35U0E1npJWfFIRMPsWFZNOvPjfLCR7TBiXlwhIGqhHUccKbRLksQhbqhL2w4xt8c1SOtTcQRcmaX9atUB3BVq9s5CNA8C9Pi1snNAbsQPggKj6Ad38V-3vuZ~maSvvuXbE64p0C3NtEWAmUnEfzBoxc877tjT7VbRorwb4W5FeRxsAst5d~4kIH-4Zvzq5TtqQMvgWGcWIjtIiIgwGvFQ8fLF40UD-hg1jwhZCwtViSsWMERuIk5JE-YAjwtg14zD0TqQGedmlZ5baW8dOc9v16UNE5MJMOCXMPS8B~KqwK4sKqjie-5tJeeQwPegN7Z-LnqAx8pUXGeJlhg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"U_Pb_geochronology_of_Variscan_granitoids_from_the_Moroccan_Meseta_Northwest_Africa_Tectonic_implications","translated_slug":"","page_count":55,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677457,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677457/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677457/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677457/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=E~y7Ty35U0E1npJWfFIRMPsWFZNOvPjfLCR7TBiXlwhIGqhHUccKbRLksQhbqhL2w4xt8c1SOtTcQRcmaX9atUB3BVq9s5CNA8C9Pi1snNAbsQPggKj6Ad38V-3vuZ~maSvvuXbE64p0C3NtEWAmUnEfzBoxc877tjT7VbRorwb4W5FeRxsAst5d~4kIH-4Zvzq5TtqQMvgWGcWIjtIiIgwGvFQ8fLF40UD-hg1jwhZCwtViSsWMERuIk5JE-YAjwtg14zD0TqQGedmlZ5baW8dOc9v16UNE5MJMOCXMPS8B~KqwK4sKqjie-5tJeeQwPegN7Z-LnqAx8pUXGeJlhg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677458,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677458/thumbnails/1.jpg","file_name":"view.pdf","download_url":"https://www.academia.edu/attachments/114677458/download_file","bulk_download_file_name":"U_Pb_geochronology_of_Variscan_granitoid.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677458/view-libre.pdf?1716014256=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_geochronology_of_Variscan_granitoid.pdf\u0026Expires=1733072613\u0026Signature=BK-fszsiA5vpMFr1zOCLEudTReoW0aEhs8Eo5VAwP03dxmhbvnlrQONZcWVsWi4qwoviaiLNsvC107l28jY-HLXkS9ONgGQRYCeU21hvyBkWeTP3IuNLv~9JziMWgLLcUyn~X24r-ZpxMcrE-P1xNFiHF9C8~Qj4HG6op8OVsIqPPgHpxL~U-8n3XykqjlgPo-xx-4CEKfxJY9KU7~1xpq9pmz08LJyeZtRc5YArzpF1LH2sXmO3y2ulJ9rtVqPVPxlss9kbQrLjdEnGbm8RP6H87J6J2dURKanxJDepJWL9SBq4yk6KDnKVXgbszI5N7ctcYJBjiHA5IFcfyMReCA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":191873,"name":"Magmatism","url":"https://www.academia.edu/Documents/in/Magmatism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065175,"url":"https://univoak.eu/islandora/object/islandora:159433/datastream/PDF/view"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267766"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile"><img alt="Research paper thumbnail of Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile" class="work-thumbnail" src="https://attachments.academia-assets.com/114677501/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile">Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile</a></div><div class="wp-workCard_item"><span>Applied Geochemistry</span><span>, Nov 1, 2020</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="22f0e43b5f9374c56a9ecd526fd86286" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677501,"asset_id":119267766,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267766"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267766"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267766; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267766]").text(description); $(".js-view-count[data-work-id=119267766]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267766; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267766']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267766, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "22f0e43b5f9374c56a9ecd526fd86286" } } $('.js-work-strip[data-work-id=119267766]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267766,"title":"Uptake of trace elements and isotope fractionation of Cu and Zn by birch (Betula pendula) growing on mineralized coal waste pile","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Aims of the present study were to determine the extent of the uptake of selected trace elements by birch (Betula pendula Roth) growing on the partly burnt coal waste pile and to evaluate isotopic fractionation of copper (Cu) zinc (Zn). Substrates, birch sap and leaves were collected in the coal waste pile and in a reference area outside the waste pile. The concentration of trace elements in birch sap and leaves both in birch growing on the coal waste pile and at reference sites increase in the range of U, As, Se \u003e Cd, Mo, Cu \u003e Pb \u003e Ba ≫ Zn. However, the uptake of elements by birch is restricted when concentration of metals in substrates are too high. Compared to the isotopic composition of Cu in waste substrates and soils (δ 65 Cu =-0.93 to + 1.49‰), this element in sap and leaves (δ 65 Cu =-0.58 to − 1.64 and-0.59 to-2.35‰, respectively) is depleted in heavy isotope regardless of plant-available concentration of Cu in substrates. Compared to the isotopic composition of Zn in substrates (δ 66 Zn =-0.20 to 1.43‰), its isotopic composition in sap and leaves (δ 66 Zn =-0.85 to + 1.00 and-0.21 to + 0.57‰, respectively) is depleted in the heavy isotope only when the plant-available concentration of Zn in the substrate and soil is high (\u003e20 mg kg − 1). At low plant-available concentration of Zn no isotopic fractionation or enrichment of Zn in the heavy isotope was recorded.","publication_date":{"day":1,"month":11,"year":2020,"errors":{}},"publication_name":"Applied Geochemistry","grobid_abstract_attachment_id":114677501},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267766/Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile","translated_internal_url":"","created_at":"2024-05-17T23:06:32.191-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677501,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677501/thumbnails/1.jpg","file_name":"j.apgeochem.2020.10474120240518-1-herkag.pdf","download_url":"https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Uptake_of_trace_elements_and_isotope_fra.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677501/j.apgeochem.2020.10474120240518-1-herkag-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DUptake_of_trace_elements_and_isotope_fra.pdf\u0026Expires=1733072613\u0026Signature=R6RB4adcwWQjvfz~DChaaqqXN639ckRpRtS0GQ3Rc4ew3sNT87UxYDW7PfSu0gu6myb9rdWCfgvACKLmJ~-m2Hmv1V~xIei8Ks~odgOE9VeqFPE48Wreb1pJcXJ~cJXC8eXpAzh1EkcTzQGk3LHpXqWjjo2fcKJrqNLXkrVx8Qw~~A8iPKt3huMq4GfTee3N9OUtC23VSypjRBtgtRSczUExxUSuJpSx1dS~1yYoCsiQI~7gZWN19-r3RzRSlGltlrJ7Zzl~kMHgbSw4RvsyuOgowGVEx0uVMoL9SpLzzFNfV9516duv~3d~pwcVBqAa1AvAr44-UdpCMYJGJOLfGQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Uptake_of_trace_elements_and_isotope_fractionation_of_Cu_and_Zn_by_birch_Betula_pendula_growing_on_mineralized_coal_waste_pile","translated_slug":"","page_count":14,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677501,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677501/thumbnails/1.jpg","file_name":"j.apgeochem.2020.10474120240518-1-herkag.pdf","download_url":"https://www.academia.edu/attachments/114677501/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Uptake_of_trace_elements_and_isotope_fra.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677501/j.apgeochem.2020.10474120240518-1-herkag-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DUptake_of_trace_elements_and_isotope_fra.pdf\u0026Expires=1733072613\u0026Signature=R6RB4adcwWQjvfz~DChaaqqXN639ckRpRtS0GQ3Rc4ew3sNT87UxYDW7PfSu0gu6myb9rdWCfgvACKLmJ~-m2Hmv1V~xIei8Ks~odgOE9VeqFPE48Wreb1pJcXJ~cJXC8eXpAzh1EkcTzQGk3LHpXqWjjo2fcKJrqNLXkrVx8Qw~~A8iPKt3huMq4GfTee3N9OUtC23VSypjRBtgtRSczUExxUSuJpSx1dS~1yYoCsiQI~7gZWN19-r3RzRSlGltlrJ7Zzl~kMHgbSw4RvsyuOgowGVEx0uVMoL9SpLzzFNfV9516duv~3d~pwcVBqAa1AvAr44-UdpCMYJGJOLfGQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":523,"name":"Chemistry","url":"https://www.academia.edu/Documents/in/Chemistry"},{"id":10743,"name":"Coal","url":"https://www.academia.edu/Documents/in/Coal"},{"id":15836,"name":"Environmental Chemistry","url":"https://www.academia.edu/Documents/in/Environmental_Chemistry"},{"id":32712,"name":"Applied Geochemistry","url":"https://www.academia.edu/Documents/in/Applied_Geochemistry"},{"id":158165,"name":"Zinc","url":"https://www.academia.edu/Documents/in/Zinc"},{"id":526952,"name":"Fractionation","url":"https://www.academia.edu/Documents/in/Fractionation"},{"id":640682,"name":"Isotope fractionation","url":"https://www.academia.edu/Documents/in/Isotope_fractionation"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element"},{"id":1035979,"name":"Betula Pendula","url":"https://www.academia.edu/Documents/in/Betula_Pendula"},{"id":1222799,"name":"Soil Water","url":"https://www.academia.edu/Documents/in/Soil_Water"},{"id":1957240,"name":"ENVIRONMENTAL SCIENCE AND MANAGEMENT","url":"https://www.academia.edu/Documents/in/ENVIRONMENTAL_SCIENCE_AND_MANAGEMENT"},{"id":3646326,"name":"Betula pubescens","url":"https://www.academia.edu/Documents/in/Betula_pubescens"}],"urls":[{"id":42065174,"url":"https://doi.org/10.1016/j.apgeochem.2020.104741"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267765"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology"><img alt="Research paper thumbnail of Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology" class="work-thumbnail" src="https://attachments.academia-assets.com/114677497/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology">Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology</a></div><div class="wp-workCard_item"><span>Lithos</span><span>, Aug 1, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="620097a1d6db74775ab0c1359433b2f5" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677497,"asset_id":119267765,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267765"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267765"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267765; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267765]").text(description); $(".js-view-count[data-work-id=119267765]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267765; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267765']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267765, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "620097a1d6db74775ab0c1359433b2f5" } } $('.js-work-strip[data-work-id=119267765]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267765,"title":"Polycyclic Palaeozoic evolution of accretionary orogenic wedge in the southern Chinese Altai: Evidence from structural relationships and U–Pb geochronology","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"Structural analysis and U-Pb geochronological study on zircons from the southern Chinese Altai (the Kalasu area, SE of the Altai city) show that the Cambro-Ordovician accretionary wedge (ca. 520-492 Ma) underwent four major geological events: 1) emplacement of Early Devonian magmas (ca. 410-400) associated with formation of a volcano-sedimentary cover, 2) major Middle Devonian (ca. 390-374 Ma) tectono-metamorphic event, 3) Late Devonian-Early Carboniferous folding without apparent metamorphism, and 4) a regional folding with localized Early Permian high-to ultrahigh-temperature reworking (ca. 300-280 Ma). The Early Devonian magmatism is characterized by emplacement of mafic rocks and granitoids in the centre of the NE-SW profile, coevally with granitoid magmatism and rhyolite volcanism in the southwest and northeast, respectively. The whole volcano-sedimentary and magmatic edifice was transposed by sub-horizontal metamorphic fabric associated with variable metamorphic degrees in different areas ranging from greenschist facies in the northeast (mu+bi±g) to amphibolite facies in the southwest (st+g±sill) and granulite facies in the centre (g+sill+kfs). This metamorphic architecture, distribution of magmatism and character of metamorphic zircon populations allow to correlate these areas with upper, middle and lower orogenic crust that developed during important vertical shortening and horizontal flow in Middle Devonian. Subsequently, the whole edifice was affected by regional NE-SW trending upright (possibly Late Devonian-Early Carboniferous) folding. Finally, Early Permian shortening produced NW-SE trending regional upright folds in the southwest and northeast and a crustal-scale vertical, tabular deformation zone in the centre. The Permian deformation is accompanied by granulite facies (kfs+cd+sill+g) metamorphism and anatexis reworking the Devonian lower orogenic crust, with extensive resetting and growth of new zircons and with intrusions of Permian granites and gabbros. This study suggests that the Early Permian event","publication_date":{"day":1,"month":8,"year":2018,"errors":{}},"publication_name":"Lithos","grobid_abstract_attachment_id":114677497},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267765/Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology","translated_internal_url":"","created_at":"2024-05-17T23:06:31.947-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677497,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677497/thumbnails/1.jpg","file_name":"709629.pdf","download_url":"https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Polycyclic_Palaeozoic_evolution_of_accre.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677497/709629-libre.pdf?1716014269=\u0026response-content-disposition=attachment%3B+filename%3DPolycyclic_Palaeozoic_evolution_of_accre.pdf\u0026Expires=1733072614\u0026Signature=e2QQkBnTW6vRZoH2eJl4J6sdLLupMqd7JS1n83tofm3tu4JIcaBQfWJXUN4cyoBeHaQPzNsyt1whonXUmNpFoZ5S3zW2gzag-e3OHPjmVNReJZXwXQcQ7tb-fMbNepTVaqu8kVmU5B4LEP0W66ZbxIWUwwkQOMaF2lLa-4CszEwZ7Ew1uSU4hruEdrOraM1hMvyh7~3eklbq5Qms4DxnF0C7ls9iq-ahWQxPLesyQTW42pLzWkKOnxi6wMW3CJRXHCV5P2~xMXtrkDSEesVxxT8dlcdZTfWTjNBDC2NB8pliX5d32BhrOuMHM2x1wnbLkzwi1C~txMym1on7premMw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Polycyclic_Palaeozoic_evolution_of_accretionary_orogenic_wedge_in_the_southern_Chinese_Altai_Evidence_from_structural_relationships_and_U_Pb_geochronology","translated_slug":"","page_count":80,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677497,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677497/thumbnails/1.jpg","file_name":"709629.pdf","download_url":"https://www.academia.edu/attachments/114677497/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Polycyclic_Palaeozoic_evolution_of_accre.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677497/709629-libre.pdf?1716014269=\u0026response-content-disposition=attachment%3B+filename%3DPolycyclic_Palaeozoic_evolution_of_accre.pdf\u0026Expires=1733072614\u0026Signature=e2QQkBnTW6vRZoH2eJl4J6sdLLupMqd7JS1n83tofm3tu4JIcaBQfWJXUN4cyoBeHaQPzNsyt1whonXUmNpFoZ5S3zW2gzag-e3OHPjmVNReJZXwXQcQ7tb-fMbNepTVaqu8kVmU5B4LEP0W66ZbxIWUwwkQOMaF2lLa-4CszEwZ7Ew1uSU4hruEdrOraM1hMvyh7~3eklbq5Qms4DxnF0C7ls9iq-ahWQxPLesyQTW42pLzWkKOnxi6wMW3CJRXHCV5P2~xMXtrkDSEesVxxT8dlcdZTfWTjNBDC2NB8pliX5d32BhrOuMHM2x1wnbLkzwi1C~txMym1on7premMw__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":3139797,"name":"Accretionary Wedge","url":"https://www.academia.edu/Documents/in/Accretionary_Wedge"}],"urls":[{"id":42065173,"url":"http://manuscript.elsevier.com/S002449371830207X/pdf/S002449371830207X.pdf"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267764"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_"><img alt="Research paper thumbnail of Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_">Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)</a></div><div class="wp-workCard_item"><span>EGUGA</span><span>, Apr 1, 2019</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267764"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267764"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267764; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267764]").text(description); $(".js-view-count[data-work-id=119267764]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267764; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267764']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267764, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267764]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267764,"title":"Active Devonian continental margin in the Variscan Bohemian Massif (the Mariánské Lázně Complex and Čistá pluton)","translated_title":"","metadata":{"publication_date":{"day":1,"month":4,"year":2019,"errors":{}},"publication_name":"EGUGA"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267764/Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mari%C3%A1nsk%C3%A9_L%C3%A1zn%C4%9B_Complex_and_%C4%8Cist%C3%A1_pluton_","translated_internal_url":"","created_at":"2024-05-17T23:06:31.741-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Active_Devonian_continental_margin_in_the_Variscan_Bohemian_Massif_the_Mariánské_Lázně_Complex_and_Čistá_pluton_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":1479595,"name":"Continental Margin","url":"https://www.academia.edu/Documents/in/Continental_Margin"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065172,"url":"http://ui.adsabs.harvard.edu/abs/2019EGUGA..2114335D/abstract"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267763"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia"><img alt="Research paper thumbnail of Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia" class="work-thumbnail" src="https://attachments.academia-assets.com/114677452/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia">Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia</a></div><div class="wp-workCard_item"><span>Šinžlèh uhaany akademijn mèdèè</span><span>, Dec 31, 2018</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="c58301af24d773c233c0083e9fb21450" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677452,"asset_id":119267763,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267763"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267763"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267763; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267763]").text(description); $(".js-view-count[data-work-id=119267763]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267763; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267763']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267763, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "c58301af24d773c233c0083e9fb21450" } } $('.js-work-strip[data-work-id=119267763]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267763,"title":"Geochemistry and geochronology of the Paleozoic sedimentary rocks in the Shar Khutul area, Central Mongolia","translated_title":"","metadata":{"publisher":"Mongolian Academy of Sciences","grobid_abstract":"The study area is located in the central part of Tsetserleg terrane in the southwestern margin of the Khangai-Khentey orogenic system. The paper presents new data on geochemistry and geochronology of sedimentary rocks from the Shar Khutul area, where the Tsetserleg terrane consists of Silurian-Devonian oceanic plate stratigraphic unit and Carboniferous shallow water sediment. The Upper Silurian to Middle Devonian Erdenetsogt Formation (S 3-D 2 er), which is an oceanic plate stratigraphic unit, is mainly composed of siliceous siltstone, volcanites, tuffs, quartzite, and cherts. The shallow water sediments are divided into Upper Devonian to Lower Carboniferous Tsetserleg Formation (D 3-C 1 cc) and Lower-Middle Carboniferous Dzargalant Formation (C 1-2 dz). The Tsetserleg Formation (D 3-C 1 cc) consists of only sedimentary rocks such as bluish-grey sandstones and siltstones, and Lower-Middle Carboniferous Dzargalant Formation (C 1-2 dz) is principally composed of medium-to coarse-grained, brown-greenish grey sandstones with thin-layers of dark siltstones and gravelites. The SiO 2 content of the Shar Khutul area sandstones ranges from 63.85 to 67.95 wt.% and the average content of TiO 2 is 0.72 wt.% and Al 2 O 3 content is 14.38 wt.%. The Chemical Index of Alteration (CIA) value ranges from 48.71 to 56.94 and the range of Index of compositional variations (ICV) is from 0.98 to 1.24. Moreover, the samples studied show that most of the sandstones are generally immature and were derived from weakly weathered source rocks. The ratios of Eu/Eu* (0.83), La/Sc (3.81), La/Co (5.30), and Cr/Th (13.81) indicate that the derivation of the Shar Khutul area sandstones from felsic rock sources and confirm the signatures of a felsic igneous provenance and suggest an active continental margin tectonic setting of the source area. The clastic zircons from the medium grained sandstone (Erdenetsogt formation) yield ages between 2.5 Ga and 236 Ma and the detrital zircons exhibit four peak ages at 1.","publication_date":{"day":31,"month":12,"year":2018,"errors":{}},"publication_name":"Šinžlèh uhaany akademijn mèdèè","grobid_abstract_attachment_id":114677452},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267763/Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia","translated_internal_url":"","created_at":"2024-05-17T23:06:31.487-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677452,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677452/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677452/1333-libre.pdf?1716014271=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=VpwT-7Sqk8pJlYpt3cYR-FDGku7qhTiFMMzEUTMkskjYgU-bWkUElgNSxCAlllRy1LgNg48EcBeB0m~f~hf0RN5UpAQbaxh6k-Pg6kv7SizPezaDiiZPsurwOio7rgp2ljoH6O1lLGAE0gtp3MSr63VbiDiCXdSxvBxpjceTrLSfK0F0yI885qibD~UmykBUS9TVRdY8BS1na868F59NkOGwLNrkFBJYeZBp2fo~7m1O1ocgpr22SYvWQaOBl~kDFxYdfCoG~dq8GoJtx0dl5NRx18Fc4-X87jkvP0z5KXjW2pCM7Yhb2Z5BJcXYIklZ~vXI~XI9WOlXJLMmuUoQSA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Geochemistry_and_geochronology_of_the_Paleozoic_sedimentary_rocks_in_the_Shar_Khutul_area_Central_Mongolia","translated_slug":"","page_count":18,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677452,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677452/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677452/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677452/1333-libre.pdf?1716014271=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=VpwT-7Sqk8pJlYpt3cYR-FDGku7qhTiFMMzEUTMkskjYgU-bWkUElgNSxCAlllRy1LgNg48EcBeB0m~f~hf0RN5UpAQbaxh6k-Pg6kv7SizPezaDiiZPsurwOio7rgp2ljoH6O1lLGAE0gtp3MSr63VbiDiCXdSxvBxpjceTrLSfK0F0yI885qibD~UmykBUS9TVRdY8BS1na868F59NkOGwLNrkFBJYeZBp2fo~7m1O1ocgpr22SYvWQaOBl~kDFxYdfCoG~dq8GoJtx0dl5NRx18Fc4-X87jkvP0z5KXjW2pCM7Yhb2Z5BJcXYIklZ~vXI~XI9WOlXJLMmuUoQSA__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"},{"id":114677453,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677453/thumbnails/1.jpg","file_name":"1333.pdf","download_url":"https://www.academia.edu/attachments/114677453/download_file","bulk_download_file_name":"Geochemistry_and_geochronology_of_the_Pa.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677453/1333-libre.pdf?1716014261=\u0026response-content-disposition=attachment%3B+filename%3DGeochemistry_and_geochronology_of_the_Pa.pdf\u0026Expires=1733072614\u0026Signature=Crd0xw22lGrWc2H~4YT7JRPYWCpqUKBokyCkh-VuU0Yxkwh1dEu~YtEBEGfFSlZD4fQMrHmjVbNn5ddq40p24Ph-xT-pHvlyQnDO1vYDsVUhVnq0xwHjzQpxDKFj5LB5tan7jpX2-RvgtPxwv0IACrSi1Ssi7JAdKkWv2QG~orLJgDG4rL2aRlMkw5TRKw18rIhGjpNok~Pxj2MiRR0NtU-CSgnj1AmtNO58hLclh7V3I~YWLZRNKzcgelcI7iZ9wmMdTC-odmb8RkOQY8gSq-TSOiAAP-tuqUOMecQFIqHrLxOMexa9ca0Os0IeTLVmYBTf6KfZTzCh-M6TG94mpQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76409,"name":"Tectonic Setting","url":"https://www.academia.edu/Documents/in/Tectonic_Setting"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":479964,"name":"Siltstone","url":"https://www.academia.edu/Documents/in/Siltstone"},{"id":976620,"name":"Sedimentary Rocks","url":"https://www.academia.edu/Documents/in/Sedimentary_Rocks"},{"id":1567560,"name":"Sedimentary Rock","url":"https://www.academia.edu/Documents/in/Sedimentary_Rock"}],"urls":[{"id":42065171,"url":"https://www.mongoliajol.info/index.php/PMAS/article/download/1045/1333"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267762"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery"><img alt="Research paper thumbnail of Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery">Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery</a></div><div class="wp-workCard_item"><span>Geoscience frontiers</span><span>, Mar 1, 2023</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267762"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267762"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267762; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267762]").text(description); $(".js-view-count[data-work-id=119267762]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267762; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267762']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267762, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267762]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267762,"title":"Anticlockwise metamorphic paths at ca. 890–790 Ma from the NE Baidrag block, Mongolia, indicate back-arc compression at the Rodinia periphery","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":3,"year":2023,"errors":{}},"publication_name":"Geoscience frontiers"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267762/Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery","translated_internal_url":"","created_at":"2024-05-17T23:06:31.247-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Anticlockwise_metamorphic_paths_at_ca_890_790_Ma_from_the_NE_Baidrag_block_Mongolia_indicate_back_arc_compression_at_the_Rodinia_periphery","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":135982,"name":"Rodinia","url":"https://www.academia.edu/Documents/in/Rodinia"},{"id":135985,"name":"Orogeny","url":"https://www.academia.edu/Documents/in/Orogeny"},{"id":166969,"name":"Gneiss","url":"https://www.academia.edu/Documents/in/Gneiss"},{"id":172299,"name":"Metamorphism","url":"https://www.academia.edu/Documents/in/Metamorphism"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":319883,"name":"Supercontinent","url":"https://www.academia.edu/Documents/in/Supercontinent"},{"id":1590367,"name":"Monazite","url":"https://www.academia.edu/Documents/in/Monazite"},{"id":1865674,"name":"Schist","url":"https://www.academia.edu/Documents/in/Schist"},{"id":3160824,"name":"Sillimanite","url":"https://www.academia.edu/Documents/in/Sillimanite"},{"id":3265172,"name":"kyanite","url":"https://www.academia.edu/Documents/in/kyanite"}],"urls":[{"id":42065170,"url":"https://doi.org/10.1016/j.gsf.2022.101520"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267761"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_"><img alt="Research paper thumbnail of Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_">Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)</a></div><div class="wp-workCard_item"><span>Geoscience frontiers</span><span>, May 1, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267761"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267761"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267761; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267761]").text(description); $(".js-view-count[data-work-id=119267761]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267761; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267761']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267761, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267761]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267761,"title":"Reconstruction of the mid-Devonian HP-HT metamorphic event in the Bohemian Massif (European Variscan belt)","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_date":{"day":1,"month":5,"year":2022,"errors":{}},"publication_name":"Geoscience frontiers"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267761/Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_","translated_internal_url":"","created_at":"2024-05-17T23:06:30.995-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Reconstruction_of_the_mid_Devonian_HP_HT_metamorphic_event_in_the_Bohemian_Massif_European_Variscan_belt_","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065169,"url":"https://doi.org/10.1016/j.gsf.2022.101374"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267760"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage"><img alt="Research paper thumbnail of From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage">From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage</a></div><div class="wp-workCard_item"><span>Gondwana Research</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267760"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267760"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267760; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267760]").text(description); $(".js-view-count[data-work-id=119267760]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267760; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267760']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267760, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267760]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267760,"title":"From Rodinian passive margin to peri-Siberian continental arc: Evidence from the multiphase Neoproterozoic–early Paleozoic magmatic record of the Zavkhan Block in the Mongolian Collage","translated_title":"","metadata":{"publisher":"Elsevier BV","publication_name":"Gondwana Research"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267760/From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage","translated_internal_url":"","created_at":"2024-05-17T23:06:30.750-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"From_Rodinian_passive_margin_to_peri_Siberian_continental_arc_Evidence_from_the_multiphase_Neoproterozoic_early_Paleozoic_magmatic_record_of_the_Zavkhan_Block_in_the_Mongolian_Collage","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":191873,"name":"Magmatism","url":"https://www.academia.edu/Documents/in/Magmatism"},{"id":319872,"name":"Continental-arc","url":"https://www.academia.edu/Documents/in/Continental-arc"},{"id":421956,"name":"Continental Crust","url":"https://www.academia.edu/Documents/in/Continental_Crust"},{"id":3382937,"name":"felsic","url":"https://www.academia.edu/Documents/in/felsic"}],"urls":[{"id":42065168,"url":"https://api.elsevier.com/content/article/PII:S1342937X23001314?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267759"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif"><img alt="Research paper thumbnail of U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif" class="work-thumbnail" src="https://attachments.academia-assets.com/114677495/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif">U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif</a></div><div class="wp-workCard_item"><span>Journal of African Earth Sciences</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="b8e24fa6e0198451f743a7369b5fab9b" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677495,"asset_id":119267759,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267759"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267759"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267759; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267759]").text(description); $(".js-view-count[data-work-id=119267759]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267759; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267759']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267759, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "b8e24fa6e0198451f743a7369b5fab9b" } } $('.js-work-strip[data-work-id=119267759]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267759,"title":"U–Pb detrital zircon geochronology and source provenance in the Moroccan Meseta (Variscan belt): A perspective from the Rehamna massif","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"HAL is a multidisciplinary open access archive for the deposit and dissemination of scientific research documents, whether they are published or not. The documents may come from teaching and research institutions in France or abroad, or from public or private research centers. L'archive ouverte pluridisciplinaire HAL, est destinée au dépôt et à la diffusion de documents scientifiques de niveau recherche, publiés ou non, émanant des établissements d'enseignement et de recherche français ou étrangers, des laboratoires publics ou privés.","publication_name":"Journal of African Earth Sciences","grobid_abstract_attachment_id":114677495},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267759/U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif","translated_internal_url":"","created_at":"2024-05-17T23:06:30.450-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677495,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677495/thumbnails/1.jpg","file_name":"20220502_Rehamna_Revised_20manuscript_HAL.pdf","download_url":"https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_detrital_zircon_geochronology_and_s.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677495/20220502_Rehamna_Revised_20manuscript_HAL-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_detrital_zircon_geochronology_and_s.pdf\u0026Expires=1733072614\u0026Signature=cGOp42YeOnwtcdgn5KveKfmiJZflp2AGeX3ykub-UhS0cdg7PH9fsqUfHW4JA8qTgtiF0~~PF1pq5fEZMLL3c0PHGQpsN2XmWLbVRXL~xkr2vmYQbHDZA8eGh9j2p6Awo~ZVs2gKm5kjYXCVa0LrNed9T-vRp19xr97WyKx38ETFR8Br1zfdmjjs30Kq0gsOHNGnTA4ec6idUawMEmcEv4fMC8eCpqG964NW-8nXCV4kHTrWqYp02dbaGqKKx0APLzffexQmuQpAQxv4A~KXrLQnqhSvgUHgUGcH2LkgaeNEUFhEMaUwuQwJYQRZoTAK6uKIGIQwC~xeFfbQyi5HZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"U_Pb_detrital_zircon_geochronology_and_source_provenance_in_the_Moroccan_Meseta_Variscan_belt_A_perspective_from_the_Rehamna_massif","translated_slug":"","page_count":39,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677495,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677495/thumbnails/1.jpg","file_name":"20220502_Rehamna_Revised_20manuscript_HAL.pdf","download_url":"https://www.academia.edu/attachments/114677495/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"U_Pb_detrital_zircon_geochronology_and_s.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677495/20220502_Rehamna_Revised_20manuscript_HAL-libre.pdf?1716014253=\u0026response-content-disposition=attachment%3B+filename%3DU_Pb_detrital_zircon_geochronology_and_s.pdf\u0026Expires=1733072614\u0026Signature=cGOp42YeOnwtcdgn5KveKfmiJZflp2AGeX3ykub-UhS0cdg7PH9fsqUfHW4JA8qTgtiF0~~PF1pq5fEZMLL3c0PHGQpsN2XmWLbVRXL~xkr2vmYQbHDZA8eGh9j2p6Awo~ZVs2gKm5kjYXCVa0LrNed9T-vRp19xr97WyKx38ETFR8Br1zfdmjjs30Kq0gsOHNGnTA4ec6idUawMEmcEv4fMC8eCpqG964NW-8nXCV4kHTrWqYp02dbaGqKKx0APLzffexQmuQpAQxv4A~KXrLQnqhSvgUHgUGcH2LkgaeNEUFhEMaUwuQwJYQRZoTAK6uKIGIQwC~xeFfbQyi5HZQ__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":14228,"name":"Geochronology","url":"https://www.academia.edu/Documents/in/Geochronology"},{"id":76748,"name":"Devonian","url":"https://www.academia.edu/Documents/in/Devonian"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":78133,"name":"Gondwana","url":"https://www.academia.edu/Documents/in/Gondwana"},{"id":96185,"name":"Carboniferous","url":"https://www.academia.edu/Documents/in/Carboniferous"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":1305086,"name":"Basement","url":"https://www.academia.edu/Documents/in/Basement"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065167,"url":"https://api.elsevier.com/content/article/PII:S1464343X22001625?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267758"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone"><img alt="Research paper thumbnail of Paleozoic geodynamics and architecture of the Mongolian Altai Zone" class="work-thumbnail" src="https://attachments.academia-assets.com/114677494/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone">Paleozoic geodynamics and architecture of the Mongolian Altai Zone</a></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="ad25b9318dc060e6aba76cdb70afc150" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677494,"asset_id":119267758,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267758"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267758"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267758; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267758]").text(description); $(".js-view-count[data-work-id=119267758]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267758; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267758']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267758, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "ad25b9318dc060e6aba76cdb70afc150" } } $('.js-work-strip[data-work-id=119267758]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267758,"title":"Paleozoic geodynamics and architecture of the Mongolian Altai Zone","translated_title":"","metadata":{"publisher":"Copernicus GmbH","publication_date":{"day":null,"month":null,"year":2022,"errors":{}}},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267758/Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone","translated_internal_url":"","created_at":"2024-05-17T23:06:30.298-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677494,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677494/thumbnails/1.jpg","file_name":"723920.pdf","download_url":"https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_geodynamics_and_architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677494/723920-libre.pdf?1716014243=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_geodynamics_and_architecture_o.pdf\u0026Expires=1733072614\u0026Signature=HBPEin89jMmIsJn83Jj6-92ZYYE0NArkVVdJtg9D-OY8x74Oar~hfQa~9hXSV5XmEhw3X5TofecJ89lOafo6ydgaOlSze89M-BLNUazGqqJqAsjLrZjeyo-KkV-g7JOSDCRmXAs9JCFpj7Ps1kb5KJzsT0afzAttzBDvzYdzOrIWqvm1vzNGN1-ktiHt445Xhh6rhb3TKaYIFtdAjsQyvaqc7WVrdjv8YZoEEyxmH1J7zai4MNja7BvjrbzZ4IoWlmfj9x~xjhuOF2IgXBOySVE6-S7cyT6dGDrAXQI0i6VEg6P8-kQPgB3TwoCEVSj-7YnEY4Cc4vHGgT9nmKzPOg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Paleozoic_geodynamics_and_architecture_of_the_Mongolian_Altai_Zone","translated_slug":"","page_count":2,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677494,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677494/thumbnails/1.jpg","file_name":"723920.pdf","download_url":"https://www.academia.edu/attachments/114677494/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Paleozoic_geodynamics_and_architecture_o.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677494/723920-libre.pdf?1716014243=\u0026response-content-disposition=attachment%3B+filename%3DPaleozoic_geodynamics_and_architecture_o.pdf\u0026Expires=1733072614\u0026Signature=HBPEin89jMmIsJn83Jj6-92ZYYE0NArkVVdJtg9D-OY8x74Oar~hfQa~9hXSV5XmEhw3X5TofecJ89lOafo6ydgaOlSze89M-BLNUazGqqJqAsjLrZjeyo-KkV-g7JOSDCRmXAs9JCFpj7Ps1kb5KJzsT0afzAttzBDvzYdzOrIWqvm1vzNGN1-ktiHt445Xhh6rhb3TKaYIFtdAjsQyvaqc7WVrdjv8YZoEEyxmH1J7zai4MNja7BvjrbzZ4IoWlmfj9x~xjhuOF2IgXBOySVE6-S7cyT6dGDrAXQI0i6VEg6P8-kQPgB3TwoCEVSj-7YnEY4Cc4vHGgT9nmKzPOg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":78102,"name":"Archean","url":"https://www.academia.edu/Documents/in/Archean"},{"id":79166,"name":"Ordovician","url":"https://www.academia.edu/Documents/in/Ordovician"},{"id":171492,"name":"Paleozoic","url":"https://www.academia.edu/Documents/in/Paleozoic"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":469741,"name":"Craton","url":"https://www.academia.edu/Documents/in/Craton"}],"urls":[]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267757"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution"><img alt="Research paper thumbnail of Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution">Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution</a></div><div class="wp-workCard_item"><span>EGUGA</span><span>, Apr 1, 2019</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267757"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267757"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267757; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267757]").text(description); $(".js-view-count[data-work-id=119267757]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267757; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267757']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267757, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267757]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267757,"title":"Geochemistry, zircon U-Pb and Hf isotopic compositions of lower crustal rocks from the Góry Sowie Massif (Central Sudetes, SW Poland): New insights on the sedimentary origin and tectono-thermal evolution","translated_title":"","metadata":{"publication_date":{"day":1,"month":4,"year":2019,"errors":{}},"publication_name":"EGUGA"},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267757/Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_G%C3%B3ry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution","translated_internal_url":"","created_at":"2024-05-17T23:06:29.756-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Geochemistry_zircon_U_Pb_and_Hf_isotopic_compositions_of_lower_crustal_rocks_from_the_Góry_Sowie_Massif_Central_Sudetes_SW_Poland_New_insights_on_the_sedimentary_origin_and_tectono_thermal_evolution","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065166,"url":"http://ui.adsabs.harvard.edu/abs/2019EGUGA..2113714T/abstract"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267756"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain"><img alt="Research paper thumbnail of Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain" class="work-thumbnail" src="https://attachments.academia-assets.com/114677492/thumbnails/1.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain">Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain</a></div><div class="wp-workCard_item"><span>Precambrian Research</span><span>, 2022</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><a id="3ec7dcd168a180c7412df210cb76ca3f" class="wp-workCard--action" rel="nofollow" data-click-track="profile-work-strip-download" data-download="{"attachment_id":114677492,"asset_id":119267756,"asset_type":"Work","button_location":"profile"}" href="https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&s=profile"><span><i class="fa fa-arrow-down"></i></span><span>Download</span></a><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267756"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267756"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267756; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267756]").text(description); $(".js-view-count[data-work-id=119267756]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267756; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267756']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267756, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (true){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "3ec7dcd168a180c7412df210cb76ca3f" } } $('.js-work-strip[data-work-id=119267756]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267756,"title":"Pre-collisional crustal evolution of the European Variscan periphery: Constraints from detrital zircon U–Pb ages and Hf isotopic record in the Precambrian metasedimentary basement of the Brunovistulian Domain","translated_title":"","metadata":{"publisher":"Elsevier BV","grobid_abstract":"In this study, U-Pb ages and Hf isotopic composition of detrital zircons from the Precambrian metasedimentary autochthon of the Brunovistulian Domain in the eastern Bohemian Massif were investigated to understand the pre-collisional evolution of the eastern periphery of the European Variscan belt. Detrital zircons of the Tonian sequences have mostly Paleoproterozoic to Neoproterozoic ages (c. 2.1-0.9 Ga) and are interpreted as detritus derived from the basement of either Baltica or Amazonia. The mostly positive ε Hf(t) values (-4 to +16) indicate a juvenile nature of their magma sources with minor older crustal components. In contrast, the Ediacaran sequences contain dominantly Neoproterozoic zircons (c. 600 Ma) and only rare Paleo-and Mesoproterozoic ages indicate that they were sourced from the adjacent Neoproterozoic magmatic arc with very limited input of recycled cratonic detritus. The large spread of ε Hf(t) values (-15 to +13) of the Neoproterozoic zircons suggests significant mixing of mantle-derived magmas with mature crustal material, typical of large continental magmatic arc systems. The zircon age patterns of the Ediacaran sequences, characterized by a dominance of the late Neoproterozoic zircons and limited Mesoproterozoic zircons, are nearly identical to those from the Teplá-Barrandian Unit and Moldanubian Zone, pointing to their similar sources. We consider such age populations as a record of sources actually exposed at the time of deposition, rather than the real provenance signature of the continental basement. The change in detrital zircon U-Pb age and Hf record of the Brunovistulian Domain took place between the early and late Neoproteorozoic, and probably reflects the plate-tectonic reconfiguration from the Rodinia formation/break-up to the evolution of the Gondwana or Baltica active margins. Our data challenge the main arguments for an existence of the Rheic oceanic suture between the Brunovistulian Domain and-Moldanubian Zone and allow for an alternative pre-collisional model of the Bohemian Massif as a single Neoproterozoic crustal domain.","publication_date":{"day":null,"month":null,"year":2022,"errors":{}},"publication_name":"Precambrian Research","grobid_abstract_attachment_id":114677492},"translated_abstract":null,"internal_url":"https://www.academia.edu/119267756/Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain","translated_internal_url":"","created_at":"2024-05-17T23:06:29.547-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[{"id":114677492,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677492/thumbnails/1.jpg","file_name":"article.pdf","download_url":"https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Pre_collisional_crustal_evolution_of_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677492/article-libre.pdf?1716014584=\u0026response-content-disposition=attachment%3B+filename%3DPre_collisional_crustal_evolution_of_the.pdf\u0026Expires=1733072614\u0026Signature=c3VvVRz9MptoHuD8oUXTpoUq8aqSWhsvC3RY1Ar5CpuXakLpPhEF2JiJRQ3293TavvUAF00nU4Im~TaXFzZUjydceT40W3s2FbCPdbJnvmf72YRyTPNAciX3zcLIaV1hoIvrjrvghZqo1Zbtl6CnBHPiZ5tyNeaolf5JH0tP8QCpT89353WAPLMG0gsL0ZpoI-O-Xh9MYsteojTzihyOWHgHaDtxGO~RiAimXN8q70n5TP4bUCwOTSOf-MISxYj2izvidr~mTtpFtWGIo757LLT~2QF1aX5fasQ66RQAHB~qfezZmkjulc70dYZqTYFQHr0BRJUOHK56LyIButVNLg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"slug":"Pre_collisional_crustal_evolution_of_the_European_Variscan_periphery_Constraints_from_detrital_zircon_U_Pb_ages_and_Hf_isotopic_record_in_the_Precambrian_metasedimentary_basement_of_the_Brunovistulian_Domain","translated_slug":"","page_count":64,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[{"id":114677492,"title":"","file_type":"pdf","scribd_thumbnail_url":"https://attachments.academia-assets.com/114677492/thumbnails/1.jpg","file_name":"article.pdf","download_url":"https://www.academia.edu/attachments/114677492/download_file?st=MTczMzA5MzQwNyw4LjIyMi4yMDguMTQ2&","bulk_download_file_name":"Pre_collisional_crustal_evolution_of_the.pdf","bulk_download_url":"https://d1wqtxts1xzle7.cloudfront.net/114677492/article-libre.pdf?1716014584=\u0026response-content-disposition=attachment%3B+filename%3DPre_collisional_crustal_evolution_of_the.pdf\u0026Expires=1733072614\u0026Signature=c3VvVRz9MptoHuD8oUXTpoUq8aqSWhsvC3RY1Ar5CpuXakLpPhEF2JiJRQ3293TavvUAF00nU4Im~TaXFzZUjydceT40W3s2FbCPdbJnvmf72YRyTPNAciX3zcLIaV1hoIvrjrvghZqo1Zbtl6CnBHPiZ5tyNeaolf5JH0tP8QCpT89353WAPLMG0gsL0ZpoI-O-Xh9MYsteojTzihyOWHgHaDtxGO~RiAimXN8q70n5TP4bUCwOTSOf-MISxYj2izvidr~mTtpFtWGIo757LLT~2QF1aX5fasQ66RQAHB~qfezZmkjulc70dYZqTYFQHr0BRJUOHK56LyIButVNLg__\u0026Key-Pair-Id=APKAJLOHF5GGSLRBV4ZA"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences"},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10477,"name":"Provenance","url":"https://www.academia.edu/Documents/in/Provenance"},{"id":78114,"name":"Precambrian","url":"https://www.academia.edu/Documents/in/Precambrian"},{"id":206457,"name":"Zircon","url":"https://www.academia.edu/Documents/in/Zircon"},{"id":579156,"name":"Detritus","url":"https://www.academia.edu/Documents/in/Detritus"},{"id":1305086,"name":"Basement","url":"https://www.academia.edu/Documents/in/Basement"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065165,"url":"https://api.elsevier.com/content/article/PII:S030192682200050X?httpAccept=text/xml"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> <div class="js-work-strip profile--work_container" data-work-id="119267755"><div class="profile--work_thumbnail hidden-xs"><a class="js-work-strip-work-link" data-click-track="profile-work-strip-thumbnail" href="https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif"><img alt="Research paper thumbnail of Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif" class="work-thumbnail" src="https://a.academia-assets.com/images/blank-paper.jpg" /></a></div><div class="wp-workCard wp-workCard_itemContainer"><div class="wp-workCard_item wp-workCard--title"><a class="js-work-strip-work-link text-gray-darker" data-click-track="profile-work-strip-title" href="https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif">Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif</a></div><div class="wp-workCard_item"><span>Journal of the Geological Society</span><span>, 2020</span></div><div class="wp-workCard_item"><span class="js-work-more-abstract-truncated">The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the interna...</span><a class="js-work-more-abstract" data-broccoli-component="work_strip.more_abstract" data-click-track="profile-work-strip-more-abstract" href="javascript:;"><span> more </span><span><i class="fa fa-caret-down"></i></span></a><span class="js-work-more-abstract-untruncated hidden">The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...</span></div><div class="wp-workCard_item wp-workCard--actions"><span class="work-strip-bookmark-button-container"></span><span class="wp-workCard--action visible-if-viewed-by-owner inline-block" style="display: none;"><span class="js-profile-work-strip-edit-button-wrapper profile-work-strip-edit-button-wrapper" data-work-id="119267755"><a class="js-profile-work-strip-edit-button" tabindex="0"><span><i class="fa fa-pencil"></i></span><span>Edit</span></a></span></span><span id="work-strip-rankings-button-container"></span></div><div class="wp-workCard_item wp-workCard--stats"><span><span><span class="js-view-count view-count u-mr2x" data-work-id="119267755"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 119267755; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=119267755]").text(description); $(".js-view-count[data-work-id=119267755]").attr('title', description).tooltip(); }); });</script></span></span><span><span class="percentile-widget hidden"><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 119267755; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-work-strip[data-work-id='119267755']"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></span><span><script>$(function() { new Works.PaperRankView({ workId: 119267755, container: "", }); });</script></span></div><div id="work-strip-premium-row-container"></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/work_edit-ad038b8c047c1a8d4fa01b402d530ff93c45fee2137a149a4a5398bc8ad67560.js"], function() { // from javascript_helper.rb var dispatcherData = {} if (false){ window.WowProfile.dispatcher = window.WowProfile.dispatcher || _.clone(Backbone.Events); dispatcherData = { dispatcher: window.WowProfile.dispatcher, downloadLinkId: "-1" } } $('.js-work-strip[data-work-id=119267755]').each(function() { if (!$(this).data('initialized')) { new WowProfile.WorkStripView({ el: this, workJSON: {"id":119267755,"title":"Tectonic significance of the Variscan suture between Brunovistulia and the Bohemian Massif","translated_title":"","metadata":{"abstract":"The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...","publisher":"Geological Society of London","publication_date":{"day":null,"month":null,"year":2020,"errors":{}},"publication_name":"Journal of the Geological Society"},"translated_abstract":"The Velké Vrbno Dome crops out at the boundary between the Brunovistulian Terrane and the internal parts of the Bohemian Massif. Here, eclogite boudins occur within an Ediacaran volcano-sedimentary sequence. Strong Nb depletion (Nb/Nb* = 0.19–0.82) combined with moderately positive Nd isotopic compositions (εNd(i) = +3.89 – +5.77) is used to argue for emplacement of the eclogite protoliths in a transitional supra-subduction to continental-rift setting. Conversely, heterogeneously enriched large ion lithophile elements and highly radiogenic Sr isotopic ratios (87Sr/86Sr = 0.705–0.720) are interpreted to have been modified following fluid infiltration subsequent to eclogite-facies metamorphism.U–Pb laser ablation inductively coupled plasma mass spectrometry dating of magmatic zircon from the rift-type eclogite indicates Early Cambrian emplacement (c. 535 Ma) following episodic Ediacaran volcanic arc activity. Moreover, a continental setting is emphasized by zircon dating of a myloniti...","internal_url":"https://www.academia.edu/119267755/Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif","translated_internal_url":"","created_at":"2024-05-17T23:06:29.345-07:00","preview_url":null,"current_user_can_edit":null,"current_user_is_owner":null,"owner_id":3753617,"coauthors_can_edit":true,"document_type":"paper","co_author_tags":[],"downloadable_attachments":[],"slug":"Tectonic_significance_of_the_Variscan_suture_between_Brunovistulia_and_the_Bohemian_Massif","translated_slug":"","page_count":null,"language":"en","content_type":"Work","owner":{"id":3753617,"first_name":"Jitka","middle_initials":null,"last_name":"Mikova","page_name":"JitkaMikova","domain_name":"czechgeologicalsurvey","created_at":"2013-04-10T23:59:14.881-07:00","display_name":"Jitka Mikova","url":"https://czechgeologicalsurvey.academia.edu/JitkaMikova"},"attachments":[],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology"},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry"},{"id":10769,"name":"Tectonics","url":"https://www.academia.edu/Documents/in/Tectonics"},{"id":4348154,"name":"Massif","url":"https://www.academia.edu/Documents/in/Massif"}],"urls":[{"id":42065164,"url":"https://syndication.highwire.org/content/doi/10.1144/jgs2020-176"}]}, dispatcherData: dispatcherData }); $(this).data('initialized', true); } }); $a.trackClickSource(".js-work-strip-work-link", "profile_work_strip") }); </script> </div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js","https://a.academia-assets.com/assets/google_contacts-0dfb882d836b94dbcb4a2d123d6933fc9533eda5be911641f20b4eb428429600.js"], function() { // from javascript_helper.rb $('.js-google-connect-button').click(function(e) { e.preventDefault(); GoogleContacts.authorize_and_show_contacts(); Aedu.Dismissibles.recordClickthrough("WowProfileImportContactsPrompt"); }); $('.js-update-biography-button').click(function(e) { e.preventDefault(); Aedu.Dismissibles.recordClickthrough("UpdateUserBiographyPrompt"); $.ajax({ url: $r.api_v0_profiles_update_about_path({ subdomain_param: 'api', about: "", }), type: 'PUT', success: function(response) { location.reload(); } }); }); $('.js-work-creator-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_document_path({ source: encodeURIComponent(""), }); }); $('.js-video-upload-button').click(function (e) { e.preventDefault(); window.location = $r.upload_funnel_video_path({ source: encodeURIComponent(""), }); }); $('.js-do-this-later-button').click(function() { $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("WowProfileImportContactsPrompt"); }); $('.js-update-biography-do-this-later-button').click(function(){ $(this).closest('.js-profile-nag-panel').remove(); Aedu.Dismissibles.recordDismissal("UpdateUserBiographyPrompt"); }); $('.wow-profile-mentions-upsell--close').click(function(){ $('.wow-profile-mentions-upsell--panel').hide(); Aedu.Dismissibles.recordDismissal("WowProfileMentionsUpsell"); }); $('.wow-profile-mentions-upsell--button').click(function(){ Aedu.Dismissibles.recordClickthrough("WowProfileMentionsUpsell"); }); new WowProfile.SocialRedesignUserWorks({ initialWorksOffset: 20, allWorksOffset: 20, maxSections: 1 }) }); </script> </div></div></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/wow_profile_edit-5ea339ee107c863779f560dd7275595239fed73f1a13d279d2b599a28c0ecd33.js","https://a.academia-assets.com/assets/add_coauthor-22174b608f9cb871d03443cafa7feac496fb50d7df2d66a53f5ee3c04ba67f53.js","https://a.academia-assets.com/assets/tab-dcac0130902f0cc2d8cb403714dd47454f11fc6fb0e99ae6a0827b06613abc20.js","https://a.academia-assets.com/assets/wow_profile-f77ea15d77ce96025a6048a514272ad8becbad23c641fc2b3bd6e24ca6ff1932.js"], function() { // from javascript_helper.rb window.ae = window.ae || {}; window.ae.WowProfile = window.ae.WowProfile || {}; if(Aedu.User.current && Aedu.User.current.id === $viewedUser.id) { window.ae.WowProfile.current_user_edit = {}; new WowProfileEdit.EditUploadView({ el: '.js-edit-upload-button-wrapper', model: window.$current_user, }); new AddCoauthor.AddCoauthorsController(); } var userInfoView = new WowProfile.SocialRedesignUserInfo({ recaptcha_key: "6LdxlRMTAAAAADnu_zyLhLg0YF9uACwz78shpjJB" }); WowProfile.router = new WowProfile.Router({ userInfoView: userInfoView }); Backbone.history.start({ pushState: true, root: "/" + $viewedUser.page_name }); new WowProfile.UserWorksNav() }); </script> </div> <div class="bootstrap login"><div class="modal fade login-modal" id="login-modal"><div class="login-modal-dialog modal-dialog"><div class="modal-content"><div class="modal-header"><button class="close close" data-dismiss="modal" type="button"><span aria-hidden="true">×</span><span class="sr-only">Close</span></button><h4 class="modal-title text-center"><strong>Log In</strong></h4></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><button class="btn btn-fb btn-lg btn-block btn-v-center-content" id="login-facebook-oauth-button"><svg style="float: left; width: 19px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="facebook-square" class="svg-inline--fa fa-facebook-square fa-w-14" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 448 512"><path fill="currentColor" d="M400 32H48A48 48 0 0 0 0 80v352a48 48 0 0 0 48 48h137.25V327.69h-63V256h63v-54.64c0-62.15 37-96.48 93.67-96.48 27.14 0 55.52 4.84 55.52 4.84v61h-31.27c-30.81 0-40.42 19.12-40.42 38.73V256h68.78l-11 71.69h-57.78V480H400a48 48 0 0 0 48-48V80a48 48 0 0 0-48-48z"></path></svg><small><strong>Log in</strong> with <strong>Facebook</strong></small></button><br /><button class="btn btn-google btn-lg btn-block btn-v-center-content" id="login-google-oauth-button"><svg style="float: left; width: 22px; line-height: 1em; margin-right: .3em;" aria-hidden="true" focusable="false" data-prefix="fab" data-icon="google-plus" class="svg-inline--fa fa-google-plus fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M256,8C119.1,8,8,119.1,8,256S119.1,504,256,504,504,392.9,504,256,392.9,8,256,8ZM185.3,380a124,124,0,0,1,0-248c31.3,0,60.1,11,83,32.3l-33.6,32.6c-13.2-12.9-31.3-19.1-49.4-19.1-42.9,0-77.2,35.5-77.2,78.1S142.3,334,185.3,334c32.6,0,64.9-19.1,70.1-53.3H185.3V238.1H302.2a109.2,109.2,0,0,1,1.9,20.7c0,70.8-47.5,121.2-118.8,121.2ZM415.5,273.8v35.5H380V273.8H344.5V238.3H380V202.8h35.5v35.5h35.2v35.5Z"></path></svg><small><strong>Log in</strong> with <strong>Google</strong></small></button><br /><style type="text/css">.sign-in-with-apple-button { width: 100%; height: 52px; border-radius: 3px; border: 1px solid black; cursor: pointer; }</style><script src="https://appleid.cdn-apple.com/appleauth/static/jsapi/appleid/1/en_US/appleid.auth.js" type="text/javascript"></script><div class="sign-in-with-apple-button" data-border="false" data-color="white" id="appleid-signin"><span   ="Sign Up with Apple" class="u-fs11"></span></div><script>AppleID.auth.init({ clientId: 'edu.academia.applesignon', scope: 'name email', redirectURI: 'https://www.academia.edu/sessions', state: "bde26a17cf3d10704c0c117cc22a23fb2d62da3a20af5538332e25ce77762c32", });</script><script>// Hacky way of checking if on fast loswp if (window.loswp == null) { (function() { const Google = window?.Aedu?.Auth?.OauthButton?.Login?.Google; const Facebook = window?.Aedu?.Auth?.OauthButton?.Login?.Facebook; if (Google) { new Google({ el: '#login-google-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } if (Facebook) { new Facebook({ el: '#login-facebook-oauth-button', rememberMeCheckboxId: 'remember_me', track: null }); } })(); }</script></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><div class="hr-heading login-hr-heading"><span class="hr-heading-text">or</span></div></div></div></div><div class="modal-body"><div class="row"><div class="col-xs-10 col-xs-offset-1"><form class="js-login-form" action="https://www.academia.edu/sessions" accept-charset="UTF-8" method="post"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><input type="hidden" name="authenticity_token" value="J45piQbZzegeAw42pIGhPz1zgdSvoAHCZsZaZ5GC5FmJo79mt78PdbWurLCggoUIYtyO63rmSKFv+OLaPWo6QQ==" autocomplete="off" /><div class="form-group"><label class="control-label" for="login-modal-email-input" style="font-size: 14px;">Email</label><input class="form-control" id="login-modal-email-input" name="login" type="email" /></div><div class="form-group"><label class="control-label" for="login-modal-password-input" style="font-size: 14px;">Password</label><input class="form-control" id="login-modal-password-input" name="password" type="password" /></div><input type="hidden" name="post_login_redirect_url" id="post_login_redirect_url" value="https://czechgeologicalsurvey.academia.edu/JitkaMikova" autocomplete="off" /><div class="checkbox"><label><input type="checkbox" name="remember_me" id="remember_me" value="1" checked="checked" /><small style="font-size: 12px; margin-top: 2px; display: inline-block;">Remember me on this computer</small></label></div><br><input type="submit" name="commit" value="Log In" class="btn btn-primary btn-block btn-lg js-login-submit" data-disable-with="Log In" /></br></form><script>typeof window?.Aedu?.recaptchaManagedForm === 'function' && window.Aedu.recaptchaManagedForm( document.querySelector('.js-login-form'), document.querySelector('.js-login-submit') );</script><small style="font-size: 12px;"><br />or <a data-target="#login-modal-reset-password-container" data-toggle="collapse" href="javascript:void(0)">reset password</a></small><div class="collapse" id="login-modal-reset-password-container"><br /><div class="well margin-0x"><form class="js-password-reset-form" action="https://www.academia.edu/reset_password" accept-charset="UTF-8" method="post"><input name="utf8" type="hidden" value="✓" autocomplete="off" /><input type="hidden" name="authenticity_token" value="Oy1vvdZDmFOnp3APk2Bs3lT/sO74ynbiqXkR9o7Zd2SVALlSZyVazgwK0omXY0jpC1C/0S2MP4GgR6lLIjGpfA==" autocomplete="off" /><p>Enter the email address you signed up with and we'll email you a reset link.</p><div class="form-group"><input class="form-control" name="email" type="email" /></div><script src="https://recaptcha.net/recaptcha/api.js" async defer></script> <script> var invisibleRecaptchaSubmit = function () { var closestForm = function (ele) { var curEle = ele.parentNode; while (curEle.nodeName !== 'FORM' && curEle.nodeName !== 'BODY'){ curEle = curEle.parentNode; } return curEle.nodeName === 'FORM' ? curEle : null }; var eles = document.getElementsByClassName('g-recaptcha'); if (eles.length > 0) { var form = closestForm(eles[0]); if (form) { form.submit(); } } }; </script> <input type="submit" data-sitekey="6Lf3KHUUAAAAACggoMpmGJdQDtiyrjVlvGJ6BbAj" data-callback="invisibleRecaptchaSubmit" class="g-recaptcha btn btn-primary btn-block" value="Email me a link" value=""/> </form></div></div><script> require.config({ waitSeconds: 90 })(["https://a.academia-assets.com/assets/collapse-45805421cf446ca5adf7aaa1935b08a3a8d1d9a6cc5d91a62a2a3a00b20b3e6a.js"], function() { // from javascript_helper.rb $("#login-modal-reset-password-container").on("shown.bs.collapse", function() { $(this).find("input[type=email]").focus(); }); }); </script> </div></div></div><div class="modal-footer"><div class="text-center"><small style="font-size: 12px;">Need an account? <a rel="nofollow" href="https://www.academia.edu/signup">Click here to sign up</a></small></div></div></div></div></div></div><script>// If we are on subdomain or non-bootstrapped page, redirect to login page instead of showing modal (function(){ if (typeof $ === 'undefined') return; var host = window.location.hostname; if ((host === $domain || host === "www."+$domain) && (typeof $().modal === 'function')) { $("#nav_log_in").click(function(e) { // Don't follow the link and open the modal e.preventDefault(); $("#login-modal").on('shown.bs.modal', function() { $(this).find("#login-modal-email-input").focus() }).modal('show'); }); } })()</script> <div class="bootstrap" id="footer"><div class="footer-content clearfix text-center padding-top-7x" style="width:100%;"><ul class="footer-links-secondary footer-links-wide list-inline margin-bottom-1x"><li><a href="https://www.academia.edu/about">About</a></li><li><a href="https://www.academia.edu/press">Press</a></li><li><a rel="nofollow" href="https://medium.com/academia">Blog</a></li><li><a href="https://www.academia.edu/documents">Papers</a></li><li><a href="https://www.academia.edu/topics">Topics</a></li><li><a href="https://www.academia.edu/journals">Academia.edu Journals</a></li><li><a rel="nofollow" href="https://www.academia.edu/hiring"><svg style="width: 13px; height: 13px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="briefcase" class="svg-inline--fa fa-briefcase fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M320 336c0 8.84-7.16 16-16 16h-96c-8.84 0-16-7.16-16-16v-48H0v144c0 25.6 22.4 48 48 48h416c25.6 0 48-22.4 48-48V288H320v48zm144-208h-80V80c0-25.6-22.4-48-48-48H176c-25.6 0-48 22.4-48 48v48H48c-25.6 0-48 22.4-48 48v80h512v-80c0-25.6-22.4-48-48-48zm-144 0H192V96h128v32z"></path></svg> <strong>We're Hiring!</strong></a></li><li><a rel="nofollow" href="https://support.academia.edu/"><svg style="width: 12px; height: 12px;" aria-hidden="true" focusable="false" data-prefix="fas" data-icon="question-circle" class="svg-inline--fa fa-question-circle fa-w-16" role="img" xmlns="http://www.w3.org/2000/svg" viewBox="0 0 512 512"><path fill="currentColor" d="M504 256c0 136.997-111.043 248-248 248S8 392.997 8 256C8 119.083 119.043 8 256 8s248 111.083 248 248zM262.655 90c-54.497 0-89.255 22.957-116.549 63.758-3.536 5.286-2.353 12.415 2.715 16.258l34.699 26.31c5.205 3.947 12.621 3.008 16.665-2.122 17.864-22.658 30.113-35.797 57.303-35.797 20.429 0 45.698 13.148 45.698 32.958 0 14.976-12.363 22.667-32.534 33.976C247.128 238.528 216 254.941 216 296v4c0 6.627 5.373 12 12 12h56c6.627 0 12-5.373 12-12v-1.333c0-28.462 83.186-29.647 83.186-106.667 0-58.002-60.165-102-116.531-102zM256 338c-25.365 0-46 20.635-46 46 0 25.364 20.635 46 46 46s46-20.636 46-46c0-25.365-20.635-46-46-46z"></path></svg> <strong>Help Center</strong></a></li></ul><ul class="footer-links-tertiary list-inline margin-bottom-1x"><li class="small">Find new research papers in:</li><li class="small"><a href="https://www.academia.edu/Documents/in/Physics">Physics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Chemistry">Chemistry</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Biology">Biology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Health_Sciences">Health Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Ecology">Ecology</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Cognitive_Science">Cognitive Science</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Mathematics">Mathematics</a></li><li class="small"><a href="https://www.academia.edu/Documents/in/Computer_Science">Computer Science</a></li></ul></div></div><div class="DesignSystem" id="credit" style="width:100%;"><ul class="u-pl0x footer-links-legal list-inline"><li><a rel="nofollow" href="https://www.academia.edu/terms">Terms</a></li><li><a rel="nofollow" href="https://www.academia.edu/privacy">Privacy</a></li><li><a rel="nofollow" href="https://www.academia.edu/copyright">Copyright</a></li><li>Academia ©2024</li></ul></div><script> //<![CDATA[ window.detect_gmtoffset = true; window.Academia && window.Academia.set_gmtoffset && Academia.set_gmtoffset('/gmtoffset'); //]]> </script> <div id='overlay_background'></div> <div id='bootstrap-modal-container' class='bootstrap'></div> <div id='ds-modal-container' class='bootstrap DesignSystem'></div> <div id='full-screen-modal'></div> </div> </body> </html>