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overflow: hidden; text-overflow: ellipsis; -webkit-line-clamp: 3; -webkit-box-orient: vertical; }</style><div class="col-xs-12 clearfix"><div class="u-floatLeft"><h1 class="PageHeader-title u-m0x u-fs30">Mineralogy</h1><div class="u-tcGrayDark">64,791 Followers</div><div class="u-tcGrayDark u-mt2x">Recent papers in <b>Mineralogy</b></div></div></div></div></div></div><div class="TabbedNavigation"><div class="container"><div class="row"><div class="col-xs-12 clearfix"><ul class="nav u-m0x u-p0x list-inline u-displayFlex"><li class="active"><a href="https://www.academia.edu/Documents/in/Mineralogy">Top Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Mineralogy/MostCited">Most Cited Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Mineralogy/MostDownloaded">Most Downloaded Papers</a></li><li><a href="https://www.academia.edu/Documents/in/Mineralogy/MostRecent">Newest Papers</a></li><li><a class="" href="https://www.academia.edu/People/Mineralogy">People</a></li></ul></div><style type="text/css">ul.nav{flex-direction:row}@media(max-width: 567px){ul.nav{flex-direction:column}.TabbedNavigation li{max-width:100%}.TabbedNavigation li.active{background-color:var(--background-grey, #dddde2)}.TabbedNavigation li.active:before,.TabbedNavigation li.active:after{display:none}}</style></div></div></div><div class="container"><div class="row"><div class="col-xs-12"><div class="u-displayFlex"><div class="u-flexGrow1"><div class="works"><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_43384269" data-work_id="43384269" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/43384269/Paulina_H%C3%AErtopanu_NEW_MINERALS_AND_MINERAL_VARIETIES_FOR_ROMANIA_NEW_MINERALS_AND_MINERAL_VARIETIES_FOR_ROMANIA">Paulina Hîrtopanu NEW MINERALS AND MINERAL VARIETIES FOR ROMANIA NEW MINERALS AND MINERAL VARIETIES FOR ROMANIA</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">Here are described new minerals and mineral varieties for Romania in the Crucea Uranium Sulfide deposit</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/43384269" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="811995577cc81ccf920a08e512ee1914" rel="nofollow" data-download="{"attachment_id":63678928,"asset_id":43384269,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/63678928/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="43580369" href="https://independent.academia.edu/PaulinaHirtopanu">Paulina Hîrtopanu</a><script data-card-contents-for-user="43580369" type="text/json">{"id":43580369,"first_name":"Paulina","last_name":"Hîrtopanu","domain_name":"independent","page_name":"PaulinaHirtopanu","display_name":"Paulina Hîrtopanu","profile_url":"https://independent.academia.edu/PaulinaHirtopanu?f_ri=414","photo":"https://0.academia-photos.com/43580369/44713670/35107015/s65_paulina.hi_rtopanu.jpg"}</script></span></span></li><li class="js-paper-rank-work_43384269 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="43384269"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 43384269, container: ".js-paper-rank-work_43384269", }); });</script></li><li class="js-percentile-work_43384269 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 43384269; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_43384269"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_43384269 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="43384269"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 43384269; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=43384269]").text(description); $(".js-view-count-work_43384269").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_43384269").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="43384269"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">2</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="251531" href="https://www.academia.edu/Documents/in/Mineralogy_Geology">Mineralogy Geology</a><script data-card-contents-for-ri="251531" type="text/json">{"id":251531,"name":"Mineralogy Geology","url":"https://www.academia.edu/Documents/in/Mineralogy_Geology?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=43384269]'), work: {"id":43384269,"title":"Paulina Hîrtopanu NEW MINERALS AND MINERAL VARIETIES FOR ROMANIA NEW MINERALS AND MINERAL VARIETIES FOR ROMANIA","created_at":"2020-06-19T05:41:11.066-07:00","url":"https://www.academia.edu/43384269/Paulina_H%C3%AErtopanu_NEW_MINERALS_AND_MINERAL_VARIETIES_FOR_ROMANIA_NEW_MINERALS_AND_MINERAL_VARIETIES_FOR_ROMANIA?f_ri=414","dom_id":"work_43384269","summary":"Here are described new minerals and mineral varieties for Romania in the Crucea Uranium Sulfide deposit","downloadable_attachments":[{"id":63678928,"asset_id":43384269,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":43580369,"first_name":"Paulina","last_name":"Hîrtopanu","domain_name":"independent","page_name":"PaulinaHirtopanu","display_name":"Paulina Hîrtopanu","profile_url":"https://independent.academia.edu/PaulinaHirtopanu?f_ri=414","photo":"https://0.academia-photos.com/43580369/44713670/35107015/s65_paulina.hi_rtopanu.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":251531,"name":"Mineralogy Geology","url":"https://www.academia.edu/Documents/in/Mineralogy_Geology?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_48585407" data-work_id="48585407" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/48585407/Structure_and_dynamics_of_partially_solidified_systems">Structure and dynamics of partially solidified systems</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Snowflakes and silicate mushes are two examples of the terrestrial regimes that may be characterized as partially solidified systems. Change of phase in clouds and magma chambers as well as in the earth&#x27;s mantle and core introduces a... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_48585407" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Snowflakes and silicate mushes are two examples of the terrestrial regimes that may be characterized as partially solidified systems. Change of phase in clouds and magma chambers as well as in the earth&#x27;s mantle and core introduces a variety of phenomena to challenge both the mathematical modeler and the experimentalist intent upon understanding the nature of such processes. Paralleling the efforts of researchers in the natural sciences, metallurgists and materials scientists have extensively investigated solidification in alloy melts to discover the controlling mechanisms for undesirable behavior such as melt segregation, freckling (Figure 1), and crystal dislocation. Unfortunately, most of the studies, whether in the geosciences or in material sciences, have focused on highly specialized problems with little or no attempt at generalizing the results or methods to other physical systems. During May 12-16, 1986, at the Stanford University Conference Center at Fallen Leaf Lake, ...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/48585407" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="3ca426d462beaed7f4287a30bd6cb80e" rel="nofollow" data-download="{"attachment_id":67120735,"asset_id":48585407,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/67120735/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="36934545" href="https://llnl.academia.edu/CharlesCarrigan">Charles Carrigan</a><script data-card-contents-for-user="36934545" type="text/json">{"id":36934545,"first_name":"Charles","last_name":"Carrigan","domain_name":"llnl","page_name":"CharlesCarrigan","display_name":"Charles Carrigan","profile_url":"https://llnl.academia.edu/CharlesCarrigan?f_ri=414","photo":"https://0.academia-photos.com/36934545/13713895/14838232/s65_charles.carrigan.jpg"}</script></span></span></li><li class="js-paper-rank-work_48585407 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="48585407"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 48585407, container: ".js-paper-rank-work_48585407", }); 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$(".js-view-count[data-work-id=48585407]").text(description); $(".js-view-count-work_48585407").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_48585407").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="48585407"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">13</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="511" href="https://www.academia.edu/Documents/in/Materials_Science">Materials Science</a>, <script data-card-contents-for-ri="511" type="text/json">{"id":511,"name":"Materials Science","url":"https://www.academia.edu/Documents/in/Materials_Science?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2404" href="https://www.academia.edu/Documents/in/Petrology">Petrology</a>, <script data-card-contents-for-ri="2404" type="text/json">{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4120" href="https://www.academia.edu/Documents/in/Crystal_Growth">Crystal Growth</a><script data-card-contents-for-ri="4120" type="text/json">{"id":4120,"name":"Crystal Growth","url":"https://www.academia.edu/Documents/in/Crystal_Growth?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=48585407]'), work: {"id":48585407,"title":"Structure and dynamics of partially solidified systems","created_at":"2021-05-04T23:52:06.336-07:00","url":"https://www.academia.edu/48585407/Structure_and_dynamics_of_partially_solidified_systems?f_ri=414","dom_id":"work_48585407","summary":"Snowflakes and silicate mushes are two examples of the terrestrial regimes that may be characterized as partially solidified systems. Change of phase in clouds and magma chambers as well as in the earth\u0026#x27;s mantle and core introduces a variety of phenomena to challenge both the mathematical modeler and the experimentalist intent upon understanding the nature of such processes. Paralleling the efforts of researchers in the natural sciences, metallurgists and materials scientists have extensively investigated solidification in alloy melts to discover the controlling mechanisms for undesirable behavior such as melt segregation, freckling (Figure 1), and crystal dislocation. Unfortunately, most of the studies, whether in the geosciences or in material sciences, have focused on highly specialized problems with little or no attempt at generalizing the results or methods to other physical systems. During May 12-16, 1986, at the Stanford University Conference Center at Fallen Leaf Lake, ...","downloadable_attachments":[{"id":67120735,"asset_id":48585407,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":36934545,"first_name":"Charles","last_name":"Carrigan","domain_name":"llnl","page_name":"CharlesCarrigan","display_name":"Charles Carrigan","profile_url":"https://llnl.academia.edu/CharlesCarrigan?f_ri=414","photo":"https://0.academia-photos.com/36934545/13713895/14838232/s65_charles.carrigan.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":511,"name":"Materials Science","url":"https://www.academia.edu/Documents/in/Materials_Science?f_ri=414","nofollow":false},{"id":2404,"name":"Petrology","url":"https://www.academia.edu/Documents/in/Petrology?f_ri=414","nofollow":false},{"id":4120,"name":"Crystal Growth","url":"https://www.academia.edu/Documents/in/Crystal_Growth?f_ri=414","nofollow":false},{"id":15989,"name":"Igneous petrology","url":"https://www.academia.edu/Documents/in/Igneous_petrology?f_ri=414"},{"id":18987,"name":"Natural Science","url":"https://www.academia.edu/Documents/in/Natural_Science?f_ri=414"},{"id":47879,"name":"National Science Foundation","url":"https://www.academia.edu/Documents/in/National_Science_Foundation?f_ri=414"},{"id":152679,"name":"Dislocations","url":"https://www.academia.edu/Documents/in/Dislocations?f_ri=414"},{"id":187673,"name":"Phase Change","url":"https://www.academia.edu/Documents/in/Phase_Change?f_ri=414"},{"id":291387,"name":"Mathematical Model","url":"https://www.academia.edu/Documents/in/Mathematical_Model?f_ri=414"},{"id":292596,"name":"North Atlantic Treaty Organization","url":"https://www.academia.edu/Documents/in/North_Atlantic_Treaty_Organization?f_ri=414"},{"id":415322,"name":"Magma Chamber","url":"https://www.academia.edu/Documents/in/Magma_Chamber?f_ri=414"},{"id":896204,"name":"Numerical Solution","url":"https://www.academia.edu/Documents/in/Numerical_Solution?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_45181234" data-work_id="45181234" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India">Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The petrography and mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy.... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_45181234" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The petrography and mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy. The petrographic and mineralogical studies also play an important role identification of various petrogenetic processes that may be responsible for producing them. In the present study an attempt has been made to understand the preliminary petrography and mineralogy of lava pile of Muktagiri. The detailed geological mapping of the study area was done, and number of filed traverses were carried out the to identify the various lava flows along with their extensions. The field specimens were collected along all the traverses. The megascopic and microscopic studies were done to identify the petrographic and mineralogical characters. About 15 lava flows were identified in the study area. These lava flows, based on mineralogical and petrographic characters were divided in to four formations namely A, B, C and D formation. Further, the lava flows can be classified into aphyric and phyric lava flows. Mineralogical study revels that the lava flows are composed of plagioclase, clinopyroxene and opaque (mostly Fe-Ti oxide). At few places places primary glass with very small proportion of olivine is also observed.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/45181234" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="f8563f3127d404d754bec9edcdd6b70f" rel="nofollow" data-download="{"attachment_id":65767064,"asset_id":45181234,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/65767064/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6079060" href="https://independent.academia.edu/IJRASETPublication">IJRASET Publication</a><script data-card-contents-for-user="6079060" type="text/json">{"id":6079060,"first_name":"IJRASET","last_name":"Publication","domain_name":"independent","page_name":"IJRASETPublication","display_name":"IJRASET Publication","profile_url":"https://independent.academia.edu/IJRASETPublication?f_ri=414","photo":"https://0.academia-photos.com/6079060/2549300/33111525/s65_ijraset.publication.jpg"}</script></span></span></li><li class="js-paper-rank-work_45181234 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="45181234"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 45181234, container: ".js-paper-rank-work_45181234", }); });</script></li><li class="js-percentile-work_45181234 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 45181234; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_45181234"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_45181234 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="45181234"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 45181234; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=45181234]").text(description); $(".js-view-count-work_45181234").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_45181234").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="45181234"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="103767" href="https://www.academia.edu/Documents/in/Petrography">Petrography</a>, <script data-card-contents-for-ri="103767" type="text/json">{"id":103767,"name":"Petrography","url":"https://www.academia.edu/Documents/in/Petrography?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="167118" href="https://www.academia.edu/Documents/in/Lava_Flows">Lava Flows</a>, <script data-card-contents-for-ri="167118" type="text/json">{"id":167118,"name":"Lava Flows","url":"https://www.academia.edu/Documents/in/Lava_Flows?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1400576" href="https://www.academia.edu/Documents/in/Deccan_Basalts">Deccan Basalts</a><script data-card-contents-for-ri="1400576" type="text/json">{"id":1400576,"name":"Deccan Basalts","url":"https://www.academia.edu/Documents/in/Deccan_Basalts?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=45181234]'), work: {"id":45181234,"title":"Preliminary Petrographic and Mineralogical Study of Muktagiri Volcanics, Betul District, M.P. [India","created_at":"2021-02-24T02:34:41.105-08:00","url":"https://www.academia.edu/45181234/Preliminary_Petrographic_and_Mineralogical_Study_of_Muktagiri_Volcanics_Betul_District_M_P_India?f_ri=414","dom_id":"work_45181234","summary":"The petrography and mineralogy form an integral part of Petrological studies of any area. The petrographical and mineralogical data is very useful in mapping and correlating the flow sequences and in establishing the flow stratigraphy. The petrographic and mineralogical studies also play an important role identification of various petrogenetic processes that may be responsible for producing them. In the present study an attempt has been made to understand the preliminary petrography and mineralogy of lava pile of Muktagiri. The detailed geological mapping of the study area was done, and number of filed traverses were carried out the to identify the various lava flows along with their extensions. The field specimens were collected along all the traverses. The megascopic and microscopic studies were done to identify the petrographic and mineralogical characters. About 15 lava flows were identified in the study area. These lava flows, based on mineralogical and petrographic characters were divided in to four formations namely A, B, C and D formation. Further, the lava flows can be classified into aphyric and phyric lava flows. Mineralogical study revels that the lava flows are composed of plagioclase, clinopyroxene and opaque (mostly Fe-Ti oxide). At few places places primary glass with very small proportion of olivine is also observed.","downloadable_attachments":[{"id":65767064,"asset_id":45181234,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6079060,"first_name":"IJRASET","last_name":"Publication","domain_name":"independent","page_name":"IJRASETPublication","display_name":"IJRASET Publication","profile_url":"https://independent.academia.edu/IJRASETPublication?f_ri=414","photo":"https://0.academia-photos.com/6079060/2549300/33111525/s65_ijraset.publication.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":103767,"name":"Petrography","url":"https://www.academia.edu/Documents/in/Petrography?f_ri=414","nofollow":false},{"id":167118,"name":"Lava Flows","url":"https://www.academia.edu/Documents/in/Lava_Flows?f_ri=414","nofollow":false},{"id":1400576,"name":"Deccan Basalts","url":"https://www.academia.edu/Documents/in/Deccan_Basalts?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_73472506" data-work_id="73472506" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/73472506/Raman_crystallographic_and_chemical_characterization_of_rom%C3%A9ite_group_minerals">Raman, crystallographic and chemical characterization of roméite-group minerals</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The roméite-group [1,2] is part of the pyrochlore supergroup and comprises some cubic oxides of A2-mB2X6-wY1-n formula in which Sb 5+ predominates in the B-site. Indices m, w and n indicate vacancies in A, X and Y crystallographic sites,... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_73472506" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The roméite-group [1,2] is part of the pyrochlore supergroup and comprises some cubic oxides of A2-mB2X6-wY1-n formula in which Sb 5+ predominates in the B-site. Indices m, w and n indicate vacancies in A, X and Y crystallographic sites, respectively. A-site is typically occupied by cations with ionic radii greater than 1.0Å or H2O, whereas X-site is usually occupied by O 2-, but smaller amounts of OHor Fare also commonly found. Finally, Y-site is typically occupied by anions O 2-, OHor F-; however, large ionic radii monovalent cations (>1.0Å) such as K + , Cs + and Rb + , or even H2O can occupy it. Since the predominance of Sb 5+ for B site is already known, the correct A and Y main occupants determine different minerals in the group and are important for the discovery of new mineral species [3]. As a source of Sb, the roméite-group minerals are economically relevant, since Sb is present in different applications, from cosmetic industry to the metal alloy production. However, only five roméite-group mineral species, namely fluorcalcioroméite, hydroxycalcioroméite, hydroxyferroroméite, oxycalcioroméite, and oxyplumboroméite have been approved by IMA. Many others can probably be discovered from possible chemical substitutions at crystallographic sites. This study analysed three different samples and determined their chemical composition by electron microprobe analysis and Raman spectra and crystal structure obtained from single-crystal X-ray diffraction. The first sample occurs in Kalugeri Hill, Babuna Valley, Jakupica Mountains, Nezilovo,Veles, Macedonia, whereas the other two occur in Prabornaz Mine, Saint Marcel, Valle d'Aosta, Italy. Sample 1 was identified as fluorcalcioroméite, and samples 2 and 3 as hydroxycalcioroméite. These are the first descriptions of these mineral species at the mentioned occurrences.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/73472506" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="75a1102d6d272eb74bba475b8b34e11d" rel="nofollow" data-download="{"attachment_id":81982459,"asset_id":73472506,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/81982459/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="151032823" href="https://ueap.academia.edu/GersonAnderson">Gerson Anderson</a><script data-card-contents-for-user="151032823" type="text/json">{"id":151032823,"first_name":"Gerson","last_name":"Anderson","domain_name":"ueap","page_name":"GersonAnderson","display_name":"Gerson Anderson","profile_url":"https://ueap.academia.edu/GersonAnderson?f_ri=414","photo":"https://0.academia-photos.com/151032823/48927022/58486478/s65_gerson.anderson.jpg"}</script></span></span></li><li class="js-paper-rank-work_73472506 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="73472506"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 73472506, container: ".js-paper-rank-work_73472506", }); 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Indices m, w and n indicate vacancies in A, X and Y crystallographic sites, respectively. A-site is typically occupied by cations with ionic radii greater than 1.0Å or H2O, whereas X-site is usually occupied by O 2-, but smaller amounts of OHor Fare also commonly found. Finally, Y-site is typically occupied by anions O 2-, OHor F-; however, large ionic radii monovalent cations (\u003e1.0Å) such as K + , Cs + and Rb + , or even H2O can occupy it. Since the predominance of Sb 5+ for B site is already known, the correct A and Y main occupants determine different minerals in the group and are important for the discovery of new mineral species [3]. As a source of Sb, the roméite-group minerals are economically relevant, since Sb is present in different applications, from cosmetic industry to the metal alloy production. However, only five roméite-group mineral species, namely fluorcalcioroméite, hydroxycalcioroméite, hydroxyferroroméite, oxycalcioroméite, and oxyplumboroméite have been approved by IMA. Many others can probably be discovered from possible chemical substitutions at crystallographic sites. This study analysed three different samples and determined their chemical composition by electron microprobe analysis and Raman spectra and crystal structure obtained from single-crystal X-ray diffraction. The first sample occurs in Kalugeri Hill, Babuna Valley, Jakupica Mountains, Nezilovo,Veles, Macedonia, whereas the other two occur in Prabornaz Mine, Saint Marcel, Valle d'Aosta, Italy. Sample 1 was identified as fluorcalcioroméite, and samples 2 and 3 as hydroxycalcioroméite. These are the first descriptions of these mineral species at the mentioned occurrences.","downloadable_attachments":[{"id":81982459,"asset_id":73472506,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":151032823,"first_name":"Gerson","last_name":"Anderson","domain_name":"ueap","page_name":"GersonAnderson","display_name":"Gerson Anderson","profile_url":"https://ueap.academia.edu/GersonAnderson?f_ri=414","photo":"https://0.academia-photos.com/151032823/48927022/58486478/s65_gerson.anderson.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":9339,"name":"Raman Spectroscopy","url":"https://www.academia.edu/Documents/in/Raman_Spectroscopy?f_ri=414","nofollow":false},{"id":9533,"name":"Minerals","url":"https://www.academia.edu/Documents/in/Minerals?f_ri=414","nofollow":false},{"id":50630,"name":"Crystal structure","url":"https://www.academia.edu/Documents/in/Crystal_structure?f_ri=414","nofollow":false},{"id":131787,"name":"XRD Crystallography","url":"https://www.academia.edu/Documents/in/XRD_Crystallography?f_ri=414"},{"id":366146,"name":"Pyrochlores","url":"https://www.academia.edu/Documents/in/Pyrochlores?f_ri=414"},{"id":411828,"name":"Minerais","url":"https://www.academia.edu/Documents/in/Minerais?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_44176344" data-work_id="44176344" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/44176344/Amazonian_Anthrosols_Support_Similar_Microbial_Communities_that_Differ_Distinctly_from_Those_Extant_in_Adjacent_Unmodified_Soils_of_the_Same_Mineralogy">Amazonian Anthrosols Support Similar Microbial Communities that Differ Distinctly from Those Extant in Adjacent, Unmodified Soils of the Same Mineralogy</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/44176344" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="bc658dcf407d71fee50fcb74483577ba" rel="nofollow" data-download="{"attachment_id":64536533,"asset_id":44176344,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button 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Microscope","url":"https://www.academia.edu/Documents/in/Scanning_Electron_Microscope?f_ri=414"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element?f_ri=414"},{"id":907289,"name":"Energy Dispersive Spectroscopy","url":"https://www.academia.edu/Documents/in/Energy_Dispersive_Spectroscopy?f_ri=414"},{"id":2803818,"name":"Atmospheric Environment","url":"https://www.academia.edu/Documents/in/Atmospheric_Environment?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_35070078" data-work_id="35070078" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/35070078/%D0%A2%D0%B5%D0%BA%D1%81%D1%82">Текст</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Rare minerals, chloriane amphiboles and chloriane biotites were discovered in rocks of Palaeoproterozoic (Jatulian) traps of Karelia: in gabbro-dolerites of layered Kojkarsko-Svjatnavolok sill and in coarse-grained albitic (“karjalitic”)... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_35070078" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Rare minerals, chloriane amphiboles and chloriane biotites were discovered in rocks of  Palaeoproterozoic (Jatulian) traps of Karelia: in gabbro-dolerites of layered Kojkarsko-Svjatnavolok sill and in coarse-grained albitic (“karjalitic”) enclave in basaltic flow, which is exposed in village Girvas. Amphiboles detected as chlorinehastingsites (AlVI  < Fe3+, Fe/(Fe2+ + Mg) > 0,6; Cl from 2,03 to 5,50%), chlorinebiotites attributed to phlogopite-annite series with Fe/Mg ≥ 0,7 and Cl content ranging from 1,44 to 3,41%. These minerals were formed at the latest subsolidus stage of crystallization of Karelian traps. The composition of them indicates high chlorine activity in late- postmagmatic fluid, which could be considered as favorable factor when evaluation of PGE metal mineralization, well known in trap layered intrusions, would be conducted.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/35070078" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="085c816cab896324f6a499532602f635" rel="nofollow" data-download="{"attachment_id":54930628,"asset_id":35070078,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/54930628/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="70975411" href="https://independent.academia.edu/MMalashin">Mikhail Malashin</a><script data-card-contents-for-user="70975411" type="text/json">{"id":70975411,"first_name":"Mikhail","last_name":"Malashin","domain_name":"independent","page_name":"MMalashin","display_name":"Mikhail Malashin","profile_url":"https://independent.academia.edu/MMalashin?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_35070078 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="35070078"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 35070078, container: ".js-paper-rank-work_35070078", }); 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Amphiboles detected as chlorinehastingsites (AlVI \u003c Fe3+, Fe/(Fe2+ + Mg) \u003e 0,6; Cl from 2,03 to 5,50%), chlorinebiotites attributed to phlogopite-annite series with Fe/Mg ≥ 0,7 and Cl content ranging from 1,44 to 3,41%. These minerals were formed at the latest subsolidus stage of crystallization of Karelian traps. The composition of them indicates high chlorine activity in late- postmagmatic fluid, which could be considered as favorable factor when evaluation of PGE metal mineralization, well known in trap layered intrusions, would be conducted.","downloadable_attachments":[{"id":54930628,"asset_id":35070078,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":70975411,"first_name":"Mikhail","last_name":"Malashin","domain_name":"independent","page_name":"MMalashin","display_name":"Mikhail Malashin","profile_url":"https://independent.academia.edu/MMalashin?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":2635,"name":"Metamorphic Petrology","url":"https://www.academia.edu/Documents/in/Metamorphic_Petrology?f_ri=414","nofollow":false},{"id":45278,"name":"Large Igneous Provinces","url":"https://www.academia.edu/Documents/in/Large_Igneous_Provinces?f_ri=414","nofollow":false},{"id":255222,"name":"Igneous and Metamorphic Petrology","url":"https://www.academia.edu/Documents/in/Igneous_and_Metamorphic_Petrology?f_ri=414"},{"id":280382,"name":"Optical Mineralogy","url":"https://www.academia.edu/Documents/in/Optical_Mineralogy?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_70110880" data-work_id="70110880" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/70110880/Reservoir_Rock_Typing_in_a_Carbonate_Reservoir_Cooperation_of_Core_and_Log_Data_Case_Study">Reservoir Rock Typing in a Carbonate Reservoir—Cooperation of Core and Log Data: Case Study</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Copyright 2009, Society of Petroleum Engineers This paper was prepared for presentation at the 2009 SPE/EAGE Reservoir Characterization and Simulation Conference held in Abu Dhabi, UAE, 1921 October 2009. This paper was selected for... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_70110880" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Copyright 2009, Society of Petroleum Engineers This paper was prepared for presentation at the 2009 SPE/EAGE Reservoir Characterization and Simulation Conference held in Abu Dhabi, UAE, 1921 October 2009. This paper was selected for presentation by an SPE ...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/70110880" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="198344" href="https://put-ir.academia.edu/RiazKharrat">Riyaz Kharrat</a><script data-card-contents-for-user="198344" type="text/json">{"id":198344,"first_name":"Riyaz","last_name":"Kharrat","domain_name":"put-ir","page_name":"RiazKharrat","display_name":"Riyaz Kharrat","profile_url":"https://put-ir.academia.edu/RiazKharrat?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_70110880 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="70110880"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 70110880, container: ".js-paper-rank-work_70110880", }); 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O objetivo deste estudo é apresentar uma lista de espécies da fauna e flora encontradas na Região da Vila Renascer, Petrolina, Estado de Pernambuco, e discutir os impactos na região, que ameaçam essa diversidade. Este estudo foi realizado a partir de entrevistas com a população local residente no entorno de uma mineradora de gnaisse, acerca dos impactos e importância da mineração. A amostragem foi aleatória, sendo selecionados 87 informantes, como critério para inclusão dos participantes na pesquisa foi adotado a idade > 18 anos e escolaridade, optando-se pelos alfabetizados. Os resultados registra que a exploração da rocha, é apontada pelos moradores como redução de espécies da fauna está o Galea spixii, o tatu Euphractus sexcinctus e cascavel Crotalus durissus terrificus pelas mudanças climáticas e pela atividade de caça desses animais e da flora Caesalpinia pyramidalis e o Spondias tuberosa devido ao desmatamento para retirada da rocha, queimadas e abertura de novas vias de acesso para mineração. Diante do exposto, a paisagem como também toda a dinâmica do meio ambiente é alterada, levando extinção de espécies da caatinga, transtornos na saúde da população e também depredação do patrimônio particular, diante disso, não se vislumbra compatibilidade entre a extração de minérios e os objetivos de proteção da fauna e da flora.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/44831534" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="6297e1c9b318ed666032eaa857381b04" rel="nofollow" data-download="{"attachment_id":65335554,"asset_id":44831534,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/65335554/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="80635189" href="https://euvoupassar.academia.edu/FredsonPereiradaSilva">Fredson Pereira da Silva</a><script data-card-contents-for-user="80635189" type="text/json">{"id":80635189,"first_name":"Fredson Pereira da","last_name":"Silva","domain_name":"euvoupassar","page_name":"FredsonPereiradaSilva","display_name":"Fredson Pereira da Silva","profile_url":"https://euvoupassar.academia.edu/FredsonPereiradaSilva?f_ri=414","photo":"https://0.academia-photos.com/80635189/19592333/20026273/s65_fredson_pereira_da.silva.jpg"}</script></span></span></li><li class="js-paper-rank-work_44831534 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="44831534"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 44831534, container: ".js-paper-rank-work_44831534", }); 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$(".js-view-count[data-work-id=44831534]").text(description); $(".js-view-count-work_44831534").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_44831534").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="44831534"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">2</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="922" href="https://www.academia.edu/Documents/in/Education">Education</a><script data-card-contents-for-ri="922" type="text/json">{"id":922,"name":"Education","url":"https://www.academia.edu/Documents/in/Education?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=44831534]'), work: {"id":44831534,"title":"Impactos sobre a conservação de recursos naturais em áreas de exploração mineral","created_at":"2021-01-04T05:52:51.660-08:00","url":"https://www.academia.edu/44831534/Impactos_sobre_a_conserva%C3%A7%C3%A3o_de_recursos_naturais_em_%C3%A1reas_de_explora%C3%A7%C3%A3o_mineral?f_ri=414","dom_id":"work_44831534","summary":" As questões que envolvem a conservação da diversidade de seres vivos no mundo vem sendo abordados frequentemente em todos os níveis de organização social, entre os temas está a extinção das espécies, como consequência das agressões ao meio ambiente, ás áreas de exploração mineral, são áreas susceptíveis a causarem dados não só ao solo, mas também a toda a diversidade de vida no local, com repercussões no seu entorno, que provoca redução ou destruição de hábitat, afugentamento da fauna, promovendo a morte de espécies da fauna e da flora terrestres e aquáticas. O objetivo deste estudo é apresentar uma lista de espécies da fauna e flora encontradas na Região da Vila Renascer, Petrolina, Estado de Pernambuco, e discutir os impactos na região, que ameaçam essa diversidade. Este estudo foi realizado a partir de entrevistas com a população local residente no entorno de uma mineradora de gnaisse, acerca dos impactos e importância da mineração. A amostragem foi aleatória, sendo selecionados 87 informantes, como critério para inclusão dos participantes na pesquisa foi adotado a idade \u003e 18 anos e escolaridade, optando-se pelos alfabetizados. Os resultados registra que a exploração da rocha, é apontada pelos moradores como redução de espécies da fauna está o Galea spixii, o tatu Euphractus sexcinctus e cascavel Crotalus durissus terrificus pelas mudanças climáticas e pela atividade de caça desses animais e da flora Caesalpinia pyramidalis e o Spondias tuberosa devido ao desmatamento para retirada da rocha, queimadas e abertura de novas vias de acesso para mineração. Diante do exposto, a paisagem como também toda a dinâmica do meio ambiente é alterada, levando extinção de espécies da caatinga, transtornos na saúde da população e também depredação do patrimônio particular, diante disso, não se vislumbra compatibilidade entre a extração de minérios e os objetivos de proteção da fauna e da flora.","downloadable_attachments":[{"id":65335554,"asset_id":44831534,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":80635189,"first_name":"Fredson Pereira da","last_name":"Silva","domain_name":"euvoupassar","page_name":"FredsonPereiradaSilva","display_name":"Fredson Pereira da Silva","profile_url":"https://euvoupassar.academia.edu/FredsonPereiradaSilva?f_ri=414","photo":"https://0.academia-photos.com/80635189/19592333/20026273/s65_fredson_pereira_da.silva.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":922,"name":"Education","url":"https://www.academia.edu/Documents/in/Education?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_44133358" data-work_id="44133358" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/44133358/PRM_10_Mineral_Pembawa_Rare_Earth">PRM 10 Mineral Pembawa Rare Earth</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">Mengenalkan Critical Raw Material (CRM) untuk MIneral Pembawa Rare Eartg</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/44133358" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c3923d78791e0b3ddf4859571dbaf2bd" rel="nofollow" data-download="{"attachment_id":64485018,"asset_id":44133358,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/64485018/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6327047" href="https://itb.academia.edu/DennyNoviansyah">Denny Noviansyah</a><script data-card-contents-for-user="6327047" type="text/json">{"id":6327047,"first_name":"Denny","last_name":"Noviansyah","domain_name":"itb","page_name":"DennyNoviansyah","display_name":"Denny Noviansyah","profile_url":"https://itb.academia.edu/DennyNoviansyah?f_ri=414","photo":"https://0.academia-photos.com/6327047/2726527/3175553/s65_denny.noviansyah.jpg"}</script></span></span></li><li class="js-paper-rank-work_44133358 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="44133358"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 44133358, container: ".js-paper-rank-work_44133358", }); });</script></li><li class="js-percentile-work_44133358 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 44133358; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_44133358"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_44133358 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="44133358"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 44133358; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=44133358]").text(description); $(".js-view-count-work_44133358").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_44133358").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="44133358"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">5</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="53910" href="https://www.academia.edu/Documents/in/Rare_Earth_Elements">Rare Earth Elements</a>, <script data-card-contents-for-ri="53910" type="text/json">{"id":53910,"name":"Rare Earth Elements","url":"https://www.academia.edu/Documents/in/Rare_Earth_Elements?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="81326" href="https://www.academia.edu/Documents/in/Industrial_Engineering_and_Management">Industrial Engineering and Management</a>, <script data-card-contents-for-ri="81326" type="text/json">{"id":81326,"name":"Industrial Engineering and Management","url":"https://www.academia.edu/Documents/in/Industrial_Engineering_and_Management?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="146671" href="https://www.academia.edu/Documents/in/Mineral_Resources">Mineral Resources</a><script data-card-contents-for-ri="146671" type="text/json">{"id":146671,"name":"Mineral Resources","url":"https://www.academia.edu/Documents/in/Mineral_Resources?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=44133358]'), work: {"id":44133358,"title":"PRM 10 Mineral Pembawa Rare Earth","created_at":"2020-09-21T07:46:16.929-07:00","url":"https://www.academia.edu/44133358/PRM_10_Mineral_Pembawa_Rare_Earth?f_ri=414","dom_id":"work_44133358","summary":"Mengenalkan Critical Raw Material (CRM) untuk MIneral Pembawa Rare Eartg","downloadable_attachments":[{"id":64485018,"asset_id":44133358,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6327047,"first_name":"Denny","last_name":"Noviansyah","domain_name":"itb","page_name":"DennyNoviansyah","display_name":"Denny Noviansyah","profile_url":"https://itb.academia.edu/DennyNoviansyah?f_ri=414","photo":"https://0.academia-photos.com/6327047/2726527/3175553/s65_denny.noviansyah.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":53910,"name":"Rare Earth Elements","url":"https://www.academia.edu/Documents/in/Rare_Earth_Elements?f_ri=414","nofollow":false},{"id":81326,"name":"Industrial Engineering and Management","url":"https://www.academia.edu/Documents/in/Industrial_Engineering_and_Management?f_ri=414","nofollow":false},{"id":146671,"name":"Mineral Resources","url":"https://www.academia.edu/Documents/in/Mineral_Resources?f_ri=414","nofollow":false},{"id":2475142,"name":"Critical Raw Materials","url":"https://www.academia.edu/Documents/in/Critical_Raw_Materials?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_35465339" data-work_id="35465339" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/35465339/On_the_mineral_characteristics_and_geochemistry_of_the_Florida_phosphate_of_Four_Corners_and_Hardee_County_mines">On the mineral characteristics and geochemistry of the Florida phosphate of Four Corners and Hardee County mines</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The Florida phosphate deposits in Four Corners and Hardee County mines are composed mainly of phosphate minerals and quartz in addition to subordinate proportions of feldspars, dolomite, calcite, gypsum, kaolinite, attapulgite and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_35465339" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The Florida phosphate deposits in Four Corners and Hardee County mines are composed mainly of phosphate minerals and quartz in addition to subordinate proportions of feldspars, dolomite, calcite, gypsum, kaolinite, attapulgite and montmorillonite. These phosphorites contain three structurally different types of mudclasts: massive mudclasts, mudclasts with concentric structure and mudclasts consisting of agglomerates of apatite mi-croparticles. The latter are represented by particles resembling phosphatized fossil bacteria associated with microbial filaments, and hollow apatite particles having surfacial coatings and connected to microbial filaments. The Florida phosphate particles are reworked and vary in mineral composition, color and shape. They are composed of a mixture of well-crystalline species including carbonate fluorapatite (francolite), carbonate apatite and fluorapatite. The color variation of the phosphate particles is related to difference in mineral composition, extent of diagenetic effects and reworking. The light-colored mudclasts are characterized by the presence of carbonate apatite and aluminum hydroxide phosphate minerals, whereas the dark mudclasts are rich in iron aluminum hydroxide phosphate minerals. The Florida phosphorites are suggested to be formed partially by authigenetic precipitation, replacement of the sea floor carbonate and diatomite, and microbial processes. With respect to elemental geochemistry, the analyzed particles contain small percentages of sulfur and iron which are related to the occurrence of pyrite. Traces of silica and alumina are recorded which may be attributed to the diagenetic. Some of the tested particles are relatively rich in phosphorous, fluorine, calcium, and magnesium, while poor in silicon, potassium and sulfur. Whereas, the bioclasts (especially teeth) are relatively rich in calcium, phosphorous and fluorine while poor in silicon, aluminum, magnesium and potassium. Hence, the microchemical analyses revealed that differential dia-genesis affected mudclasts more than bioclasts. There is a complete compositional gradation between clay and phosphate particles which reflects their interaction. This involved kaolinitization of the phosphate particles, phosphatization of the clay mineral particles and production of silica.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/35465339" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="55fcf98d2a66afdca1517e8d1ff2c82c" rel="nofollow" data-download="{"attachment_id":55327654,"asset_id":35465339,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/55327654/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6825888" href="https://independent.academia.edu/FaresHowari">Fares Howari</a><script data-card-contents-for-user="6825888" type="text/json">{"id":6825888,"first_name":"Fares","last_name":"Howari","domain_name":"independent","page_name":"FaresHowari","display_name":"Fares Howari","profile_url":"https://independent.academia.edu/FaresHowari?f_ri=414","photo":"https://0.academia-photos.com/6825888/3034743/3566345/s65_fares.howari.jpg"}</script></span></span></li><li class="js-paper-rank-work_35465339 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="35465339"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 35465339, container: ".js-paper-rank-work_35465339", }); 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$(".js-view-count[data-work-id=35465339]").text(description); $(".js-view-count-work_35465339").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_35465339").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="35465339"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="15987" href="https://www.academia.edu/Documents/in/Phosphate_Analysis">Phosphate Analysis</a>, <script data-card-contents-for-ri="15987" type="text/json">{"id":15987,"name":"Phosphate Analysis","url":"https://www.academia.edu/Documents/in/Phosphate_Analysis?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="16937" href="https://www.academia.edu/Documents/in/Petrology_and_Geochemistry">Petrology and Geochemistry</a><script data-card-contents-for-ri="16937" type="text/json">{"id":16937,"name":"Petrology and Geochemistry","url":"https://www.academia.edu/Documents/in/Petrology_and_Geochemistry?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=35465339]'), work: {"id":35465339,"title":"On the mineral characteristics and geochemistry of the Florida phosphate of Four Corners and Hardee County mines","created_at":"2017-12-19T01:21:35.865-08:00","url":"https://www.academia.edu/35465339/On_the_mineral_characteristics_and_geochemistry_of_the_Florida_phosphate_of_Four_Corners_and_Hardee_County_mines?f_ri=414","dom_id":"work_35465339","summary":"The Florida phosphate deposits in Four Corners and Hardee County mines are composed mainly of phosphate minerals and quartz in addition to subordinate proportions of feldspars, dolomite, calcite, gypsum, kaolinite, attapulgite and montmorillonite. These phosphorites contain three structurally different types of mudclasts: massive mudclasts, mudclasts with concentric structure and mudclasts consisting of agglomerates of apatite mi-croparticles. The latter are represented by particles resembling phosphatized fossil bacteria associated with microbial filaments, and hollow apatite particles having surfacial coatings and connected to microbial filaments. The Florida phosphate particles are reworked and vary in mineral composition, color and shape. They are composed of a mixture of well-crystalline species including carbonate fluorapatite (francolite), carbonate apatite and fluorapatite. The color variation of the phosphate particles is related to difference in mineral composition, extent of diagenetic effects and reworking. The light-colored mudclasts are characterized by the presence of carbonate apatite and aluminum hydroxide phosphate minerals, whereas the dark mudclasts are rich in iron aluminum hydroxide phosphate minerals. The Florida phosphorites are suggested to be formed partially by authigenetic precipitation, replacement of the sea floor carbonate and diatomite, and microbial processes. With respect to elemental geochemistry, the analyzed particles contain small percentages of sulfur and iron which are related to the occurrence of pyrite. Traces of silica and alumina are recorded which may be attributed to the diagenetic. Some of the tested particles are relatively rich in phosphorous, fluorine, calcium, and magnesium, while poor in silicon, potassium and sulfur. Whereas, the bioclasts (especially teeth) are relatively rich in calcium, phosphorous and fluorine while poor in silicon, aluminum, magnesium and potassium. Hence, the microchemical analyses revealed that differential dia-genesis affected mudclasts more than bioclasts. There is a complete compositional gradation between clay and phosphate particles which reflects their interaction. This involved kaolinitization of the phosphate particles, phosphatization of the clay mineral particles and production of silica.","downloadable_attachments":[{"id":55327654,"asset_id":35465339,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":6825888,"first_name":"Fares","last_name":"Howari","domain_name":"independent","page_name":"FaresHowari","display_name":"Fares Howari","profile_url":"https://independent.academia.edu/FaresHowari?f_ri=414","photo":"https://0.academia-photos.com/6825888/3034743/3566345/s65_fares.howari.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":15987,"name":"Phosphate Analysis","url":"https://www.academia.edu/Documents/in/Phosphate_Analysis?f_ri=414","nofollow":false},{"id":16937,"name":"Petrology and Geochemistry","url":"https://www.academia.edu/Documents/in/Petrology_and_Geochemistry?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_15713088 coauthored" data-work_id="15713088" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/15713088/Repeatability_analysis_of_land_time_lapse_seismic_data_CO2CRC_Otway_pilot_project_case_study">Repeatability analysis of land time-lapse seismic data: CO2CRC Otway pilot project case study</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/15713088" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="89dfdbfab5d78e6ac5679df528f765ec" rel="nofollow" data-download="{"attachment_id":42945143,"asset_id":15713088,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/42945143/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="34902100" href="https://independent.academia.edu/Kepic">A. Kepic</a><script data-card-contents-for-user="34902100" type="text/json">{"id":34902100,"first_name":"A.","last_name":"Kepic","domain_name":"independent","page_name":"Kepic","display_name":"A. Kepic","profile_url":"https://independent.academia.edu/Kepic?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-15713088">+2</span><div class="hidden js-additional-users-15713088"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/UrosevicM">M. Urosevic</a></span></div><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://independent.academia.edu/RPevzner">R. 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Kepic","profile_url":"https://independent.academia.edu/Kepic?f_ri=414","photo":"/images/s65_no_pic.png"},{"id":35345108,"first_name":"M.","last_name":"Urosevic","domain_name":"independent","page_name":"UrosevicM","display_name":"M. Urosevic","profile_url":"https://independent.academia.edu/UrosevicM?f_ri=414","photo":"/images/s65_no_pic.png"},{"id":34724429,"first_name":"R.","last_name":"Pevzner","domain_name":"independent","page_name":"RPevzner","display_name":"R. Pevzner","profile_url":"https://independent.academia.edu/RPevzner?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":403,"name":"Gemology","url":"https://www.academia.edu/Documents/in/Gemology?f_ri=414","nofollow":false},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":408,"name":"Geomorphology","url":"https://www.academia.edu/Documents/in/Geomorphology?f_ri=414","nofollow":false},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=414"},{"id":410,"name":"Glaciology","url":"https://www.academia.edu/Documents/in/Glaciology?f_ri=414"},{"id":411,"name":"Hydrogeology","url":"https://www.academia.edu/Documents/in/Hydrogeology?f_ri=414"},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414"},{"id":417,"name":"Paleontology","url":"https://www.academia.edu/Documents/in/Paleontology?f_ri=414"},{"id":421,"name":"Soil 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Study","url":"https://www.academia.edu/Documents/in/Case_Study?f_ri=414"},{"id":144378,"name":"Projects","url":"https://www.academia.edu/Documents/in/Projects?f_ri=414"},{"id":189276,"name":"Offshore","url":"https://www.academia.edu/Documents/in/Offshore?f_ri=414"},{"id":191873,"name":"Magmatism","url":"https://www.academia.edu/Documents/in/Magmatism?f_ri=414"},{"id":193156,"name":"Reservoirs","url":"https://www.academia.edu/Documents/in/Reservoirs?f_ri=414"},{"id":417165,"name":"Volcanism","url":"https://www.academia.edu/Documents/in/Volcanism?f_ri=414"},{"id":505937,"name":"Regional Geology","url":"https://www.academia.edu/Documents/in/Regional_Geology?f_ri=414"},{"id":581258,"name":"Hazards","url":"https://www.academia.edu/Documents/in/Hazards?f_ri=414"},{"id":952972,"name":"Folds","url":"https://www.academia.edu/Documents/in/Folds?f_ri=414"},{"id":991311,"name":"Signal to Noise Ratio","url":"https://www.academia.edu/Documents/in/Signal_to_Noise_Ratio?f_ri=414"},{"id":1318481,"name":"Pilot project","url":"https://www.academia.edu/Documents/in/Pilot_project?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_17802318" data-work_id="17802318" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/17802318/Retrograde_formation_of_NaCl_scapolite_in_high_pressure_metaevaporites_from_the_Cordilleras_B_ticas_Spain_">Retrograde formation of NaCl-scapolite in high pressure metaevaporites from the Cordilleras B�ticas (Spain)</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a 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href="https://www.academia.edu/64289232/Skeletal_mineralogy_in_a_high_CO2_world">Skeletal mineralogy in a high-CO2 world</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/64289232" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="0901a297bfba4872e355da0efa7bd124" rel="nofollow" data-download="{"attachment_id":76391946,"asset_id":64289232,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" 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class="js-paper-rank-work_64289232 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="64289232"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 64289232, container: ".js-paper-rank-work_64289232", }); });</script></li><li class="js-percentile-work_64289232 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 64289232; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_64289232"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_64289232 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="64289232"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 64289232; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=64289232]").text(description); $(".js-view-count-work_64289232").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_64289232").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="64289232"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">11</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="3855" href="https://www.academia.edu/Documents/in/Polymorphism">Polymorphism</a>, <script data-card-contents-for-ri="3855" type="text/json">{"id":3855,"name":"Polymorphism","url":"https://www.academia.edu/Documents/in/Polymorphism?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="7710" href="https://www.academia.edu/Documents/in/Biology">Biology</a>, <script data-card-contents-for-ri="7710" type="text/json">{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="47884" href="https://www.academia.edu/Documents/in/Biological_Sciences">Biological Sciences</a><script data-card-contents-for-ri="47884" type="text/json">{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=64289232]'), work: {"id":64289232,"title":"Skeletal mineralogy in a high-CO2 world","created_at":"2021-12-15T06:09:35.685-08:00","url":"https://www.academia.edu/64289232/Skeletal_mineralogy_in_a_high_CO2_world?f_ri=414","dom_id":"work_64289232","summary":null,"downloadable_attachments":[{"id":76391946,"asset_id":64289232,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":71096661,"first_name":"Justin","last_name":"Ries","domain_name":"independent","page_name":"JustinRies","display_name":"Justin Ries","profile_url":"https://independent.academia.edu/JustinRies?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":3855,"name":"Polymorphism","url":"https://www.academia.edu/Documents/in/Polymorphism?f_ri=414","nofollow":false},{"id":7710,"name":"Biology","url":"https://www.academia.edu/Documents/in/Biology?f_ri=414","nofollow":false},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=414","nofollow":false},{"id":58054,"name":"Environmental Sciences","url":"https://www.academia.edu/Documents/in/Environmental_Sciences?f_ri=414"},{"id":68527,"name":"Ocean acidification","url":"https://www.academia.edu/Documents/in/Ocean_acidification?f_ri=414"},{"id":73606,"name":"World","url":"https://www.academia.edu/Documents/in/World?f_ri=414"},{"id":93298,"name":"Fossil Fuels","url":"https://www.academia.edu/Documents/in/Fossil_Fuels?f_ri=414"},{"id":201604,"name":"Skeleton","url":"https://www.academia.edu/Documents/in/Skeleton?f_ri=414"},{"id":276809,"name":"Shell","url":"https://www.academia.edu/Documents/in/Shell?f_ri=414"},{"id":526952,"name":"Fractionation","url":"https://www.academia.edu/Documents/in/Fractionation?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_31723194" data-work_id="31723194" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/31723194/LEVANTAMIENTO_GEOL%C3%93GICO_DE_SUPERFICIE_AL_NORTE_DEL_SECTOR_EL_AN%C3%8DS_ESTADO_M%C3%89RIDA_CUENCAS_LA_HONDA_Y_MOR%C3%93N_SURFACE_GEOLOGICAL_UPLIFT_AT_EL_ANIS_NORTH_SECTOR_M%C3%89RIDA_STATE_LA_HONDA_AND_MORON_BASINS">LEVANTAMIENTO GEOLÓGICO DE SUPERFICIE AL NORTE DEL SECTOR EL ANÍS, ESTADO MÉRIDA: CUENCAS LA HONDA Y MORÓN. SURFACE GEOLOGICAL UPLIFT AT EL ANIS NORTH SECTOR, MÉRIDA STATE: LA HONDA AND MORON BASINS</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">Campo durante tres semanas en la Zona Chiguará - El Anís.</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/31723194" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="a760c4844659dd82a699f04ec4fa2f0b" rel="nofollow" data-download="{"attachment_id":52035017,"asset_id":31723194,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/52035017/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="61034870" href="https://independent.academia.edu/NoreSoto">Nore Soto</a><script data-card-contents-for-user="61034870" type="text/json">{"id":61034870,"first_name":"Nore","last_name":"Soto","domain_name":"independent","page_name":"NoreSoto","display_name":"Nore Soto","profile_url":"https://independent.academia.edu/NoreSoto?f_ri=414","photo":"https://0.academia-photos.com/61034870/19936082/19736628/s65_nore.soto.jpg"}</script></span></span></li><li class="js-paper-rank-work_31723194 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="31723194"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 31723194, container: ".js-paper-rank-work_31723194", }); 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$(".js-view-count[data-work-id=31723194]").text(description); $(".js-view-count-work_31723194").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_31723194").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="31723194"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="48807" href="https://www.academia.edu/Documents/in/Sedimentary_geology_and_stratigraphy">Sedimentary geology and stratigraphy</a>, <script data-card-contents-for-ri="48807" type="text/json">{"id":48807,"name":"Sedimentary geology and stratigraphy","url":"https://www.academia.edu/Documents/in/Sedimentary_geology_and_stratigraphy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="366310" href="https://www.academia.edu/Documents/in/Geologia_Estrutural">Geologia Estrutural</a><script data-card-contents-for-ri="366310" type="text/json">{"id":366310,"name":"Geologia Estrutural","url":"https://www.academia.edu/Documents/in/Geologia_Estrutural?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=31723194]'), work: {"id":31723194,"title":"LEVANTAMIENTO GEOLÓGICO DE SUPERFICIE AL NORTE DEL SECTOR EL ANÍS, ESTADO MÉRIDA: CUENCAS LA HONDA Y MORÓN. SURFACE GEOLOGICAL UPLIFT AT EL ANIS NORTH SECTOR, MÉRIDA STATE: LA HONDA AND MORON BASINS","created_at":"2017-03-05T12:34:39.066-08:00","url":"https://www.academia.edu/31723194/LEVANTAMIENTO_GEOL%C3%93GICO_DE_SUPERFICIE_AL_NORTE_DEL_SECTOR_EL_AN%C3%8DS_ESTADO_M%C3%89RIDA_CUENCAS_LA_HONDA_Y_MOR%C3%93N_SURFACE_GEOLOGICAL_UPLIFT_AT_EL_ANIS_NORTH_SECTOR_M%C3%89RIDA_STATE_LA_HONDA_AND_MORON_BASINS?f_ri=414","dom_id":"work_31723194","summary":"Campo durante tres semanas en la Zona Chiguará - El Anís. ","downloadable_attachments":[{"id":52035017,"asset_id":31723194,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":61034870,"first_name":"Nore","last_name":"Soto","domain_name":"independent","page_name":"NoreSoto","display_name":"Nore Soto","profile_url":"https://independent.academia.edu/NoreSoto?f_ri=414","photo":"https://0.academia-photos.com/61034870/19936082/19736628/s65_nore.soto.jpg"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":48807,"name":"Sedimentary geology and stratigraphy","url":"https://www.academia.edu/Documents/in/Sedimentary_geology_and_stratigraphy?f_ri=414","nofollow":false},{"id":366310,"name":"Geologia Estrutural","url":"https://www.academia.edu/Documents/in/Geologia_Estrutural?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_28722518" data-work_id="28722518" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/28722518/MINERALES_Elementos_Nativos_y_Sulfuros_">MINERALES (Elementos Nativos y Sulfuros)</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/28722518" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="60112ee2996affa989fddad85a3c4bf0" rel="nofollow" data-download="{"attachment_id":49129467,"asset_id":28722518,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49129467/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="54023050" href="https://independent.academia.edu/SantiagoGaviriaMaya">Santiago Gaviria Maya</a><script data-card-contents-for-user="54023050" type="text/json">{"id":54023050,"first_name":"Santiago","last_name":"Gaviria Maya","domain_name":"independent","page_name":"SantiagoGaviriaMaya","display_name":"Santiago Gaviria Maya","profile_url":"https://independent.academia.edu/SantiagoGaviriaMaya?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_28722518 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="28722518"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 28722518, container: ".js-paper-rank-work_28722518", }); });</script></li><li class="js-percentile-work_28722518 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 28722518; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_28722518"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_28722518 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="28722518"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 28722518; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=28722518]").text(description); $(".js-view-count-work_28722518").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_28722518").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="28722518"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i></div><span class="InlineList-item-text u-textTruncate u-pl6x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a><script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (false) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=28722518]'), work: {"id":28722518,"title":"MINERALES (Elementos Nativos y Sulfuros)","created_at":"2016-09-26T06:37:15.584-07:00","url":"https://www.academia.edu/28722518/MINERALES_Elementos_Nativos_y_Sulfuros_?f_ri=414","dom_id":"work_28722518","summary":null,"downloadable_attachments":[{"id":49129467,"asset_id":28722518,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":54023050,"first_name":"Santiago","last_name":"Gaviria Maya","domain_name":"independent","page_name":"SantiagoGaviriaMaya","display_name":"Santiago Gaviria Maya","profile_url":"https://independent.academia.edu/SantiagoGaviriaMaya?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_16594966" data-work_id="16594966" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/16594966/MICROAN%C3%81LISIS_POR_DISPERSI%C3%93N_DE_ENERG%C3%8DA_XPS_DE_ESPELEOTEMAS_DE_YESO_Y_%C3%93PALO_A_EN_UNA_CUEVA_EN_ARENISCA_DE_JAIZKIBEL_PA%C3%8DS_VASCO_">MICROANÁLISIS POR DISPERSIÓN DE ENERGÍA XPS DE ESPELEOTEMAS DE YESO Y ÓPALO-A EN UNA CUEVA EN ARENISCA DE JAIZKIBEL (PAÍS VASCO)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">We present new data about speleothems of gypsum formerly analyzed by DRX. These speleothems are located in a cave in carbonatic sandstone of the Jaizkibel Formation (of Eocene age). The sample has been analyzed by an energy dispersion... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_16594966" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">We present new data about speleothems of gypsum formerly analyzed by DRX. These speleothems are located in a cave in carbonatic sandstone of the Jaizkibel Formation (of Eocene age). The sample has been analyzed by an energy dispersion microanalyzer (XPS) connected to the equipment of a scanning electron microscopy (SEM). The acicular crystals of gypsum grow on a basis of opal-A. In addition, there are traces of other elements, as C, which we attribute to organic matter from microbial mats adjoining to the speleothems.<br />Link: <a href="http://www.aranzadi.eus/fileadmin/webs/Publicaciones/pdfs/GREEN%20CAVE4.pdf" rel="nofollow">http://www.aranzadi.eus/fileadmin/webs/Publicaciones/pdfs/GREEN%20CAVE4.pdf</a></div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/16594966" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="834ffecdcca60e0e670c1c534b8b8910" rel="nofollow" data-download="{"attachment_id":39067621,"asset_id":16594966,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/39067621/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="2646995" href="https://metaaprendizaje.academia.edu/CarlosGal%C3%A1n">Carlos Galán</a><script data-card-contents-for-user="2646995" type="text/json">{"id":2646995,"first_name":"Carlos","last_name":"Galán","domain_name":"metaaprendizaje","page_name":"CarlosGalán","display_name":"Carlos Galán","profile_url":"https://metaaprendizaje.academia.edu/CarlosGal%C3%A1n?f_ri=414","photo":"https://0.academia-photos.com/2646995/843592/1048425/s65_carlos.gal_n.jpg"}</script></span></span></li><li class="js-paper-rank-work_16594966 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="16594966"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 16594966, container: ".js-paper-rank-work_16594966", }); 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$(".js-view-count[data-work-id=16594966]").text(description); $(".js-view-count-work_16594966").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_16594966").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="16594966"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">9</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="47884" href="https://www.academia.edu/Documents/in/Biological_Sciences">Biological Sciences</a>, <script data-card-contents-for-ri="47884" type="text/json">{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="62039" href="https://www.academia.edu/Documents/in/Karst_and_speleology">Karst and speleology</a>, <script data-card-contents-for-ri="62039" type="text/json">{"id":62039,"name":"Karst and speleology","url":"https://www.academia.edu/Documents/in/Karst_and_speleology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="106896" href="https://www.academia.edu/Documents/in/Cave_and_Karst_Studies">Cave and Karst Studies</a><script data-card-contents-for-ri="106896" type="text/json">{"id":106896,"name":"Cave and Karst Studies","url":"https://www.academia.edu/Documents/in/Cave_and_Karst_Studies?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=16594966]'), work: {"id":16594966,"title":"MICROANÁLISIS POR DISPERSIÓN DE ENERGÍA XPS DE ESPELEOTEMAS DE YESO Y ÓPALO-A EN UNA CUEVA EN ARENISCA DE JAIZKIBEL (PAÍS VASCO)","created_at":"2015-10-09T04:25:24.682-07:00","url":"https://www.academia.edu/16594966/MICROAN%C3%81LISIS_POR_DISPERSI%C3%93N_DE_ENERG%C3%8DA_XPS_DE_ESPELEOTEMAS_DE_YESO_Y_%C3%93PALO_A_EN_UNA_CUEVA_EN_ARENISCA_DE_JAIZKIBEL_PA%C3%8DS_VASCO_?f_ri=414","dom_id":"work_16594966","summary":"We present new data about speleothems of gypsum formerly analyzed by DRX. These speleothems are located in a cave in carbonatic sandstone of the Jaizkibel Formation (of Eocene age). The sample has been analyzed by an energy dispersion microanalyzer (XPS) connected to the equipment of a scanning electron microscopy (SEM). The acicular crystals of gypsum grow on a basis of opal-A. In addition, there are traces of other elements, as C, which we attribute to organic matter from microbial mats adjoining to the speleothems.\nLink: http://www.aranzadi.eus/fileadmin/webs/Publicaciones/pdfs/GREEN%20CAVE4.pdf\n","downloadable_attachments":[{"id":39067621,"asset_id":16594966,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":2646995,"first_name":"Carlos","last_name":"Galán","domain_name":"metaaprendizaje","page_name":"CarlosGalán","display_name":"Carlos Galán","profile_url":"https://metaaprendizaje.academia.edu/CarlosGal%C3%A1n?f_ri=414","photo":"https://0.academia-photos.com/2646995/843592/1048425/s65_carlos.gal_n.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":47884,"name":"Biological Sciences","url":"https://www.academia.edu/Documents/in/Biological_Sciences?f_ri=414","nofollow":false},{"id":62039,"name":"Karst and speleology","url":"https://www.academia.edu/Documents/in/Karst_and_speleology?f_ri=414","nofollow":false},{"id":106896,"name":"Cave and Karst Studies","url":"https://www.academia.edu/Documents/in/Cave_and_Karst_Studies?f_ri=414","nofollow":false},{"id":180056,"name":"Gypsum","url":"https://www.academia.edu/Documents/in/Gypsum?f_ri=414"},{"id":559425,"name":"Opal-A Speleothems","url":"https://www.academia.edu/Documents/in/Opal-A_Speleothems?f_ri=414"},{"id":783432,"name":"Biological activity","url":"https://www.academia.edu/Documents/in/Biological_activity?f_ri=414"},{"id":858051,"name":"Sandstone Caves","url":"https://www.academia.edu/Documents/in/Sandstone_Caves?f_ri=414"},{"id":2039496,"name":"Pseudokarst in sandstone","url":"https://www.academia.edu/Documents/in/Pseudokarst_in_sandstone?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_5808980" data-work_id="5808980" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/5808980/Chemical_heterogeneity_in_an_enderbite_hosted_pseudotachylite_eastern_India_evidence_for_syn_deformation_multi_reaction_melting_in_pseudotachylite">Chemical heterogeneity in an enderbite-hosted pseudotachylite, eastern India: evidence for syn-deformation multi-reaction melting in pseudotachylite</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The origin of chemical and mineralogical heterogeneity in tens-of-microns wide layers and domains in enderbite-hosted couple-of-centimeters wide pseudotachylite vein is examined based on the results of BSE and X-ray element imaging, and... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_5808980" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The origin of chemical and mineralogical heterogeneity in tens-of-microns wide layers and domains in enderbite-hosted couple-of-centimeters wide pseudotachylite vein is examined based on the results of BSE and X-ray element imaging, and electron probe microanalyses of major elements of host-rock minerals, clasts, microphenocrysts, and pseudotachylite matrix. The pseudotachylite layers and domains containing variable proportions of orthopyroxene and magnetite microphenocrysts continue as mantles around quartz, K-feldspar, plagioclase and garnet clasts. The clasts are chemically modified along margins and intra-clast pseudotachylite injections. The chemical modifications are extensive in smaller clasts <5 μm diameter. At least three chemically distinct layers and domains in the pseudotachylite, and their fine-grained matrices, plot in sharply defined, well-segregated and non-overlapping fields in FeO + MgO−Al2O3–SiO2, FeO–CaO–MgO and CaO–Na2O–K2O and FeO vs. FeO/FeO + MgO diagrams. The compositions of the layers and domains—smeared between a feldspar + quartz component and a ferromagnesian component of garnet + Fe–Ti oxides (±orthopyroxene)—possibly correspond to fractionated quenched melts, or admixtures of microphenocrysts that cannot be resolved by the microbeam techniques employed. The compositional variations are incompatible with deformation-driven crystal fractionation in melt. Instead the layers and domains possibly are crystal-melt mushes produced by syn-deformation ultra-high temperature (1,250–1,375°C) melting reactions involving variable proportions of host-rock minerals determined by time-transient local phase aggregates experiencing strain. The similar element variation trends in pseudotachylite examined here and those reported from anorthosite, metapelite and charnockite elsewhere suggests local phase aggregate controlled multi-reaction melting is a phenomenon commoner than hitherto realized in pseudotachylites.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/5808980" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="3a0e0c17a52f2c6fc5e7a96faef18780" rel="nofollow" data-download="{"attachment_id":49129817,"asset_id":5808980,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49129817/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="8522268" href="https://du-in.academia.edu/NareshPant">Naresh Pant</a><script data-card-contents-for-user="8522268" type="text/json">{"id":8522268,"first_name":"Naresh","last_name":"Pant","domain_name":"du-in","page_name":"NareshPant","display_name":"Naresh Pant","profile_url":"https://du-in.academia.edu/NareshPant?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_5808980 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="5808980"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 5808980, container: ".js-paper-rank-work_5808980", }); 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The pseudotachylite layers and domains containing variable proportions of orthopyroxene and magnetite microphenocrysts continue as mantles around quartz, K-feldspar, plagioclase and garnet clasts. The clasts are chemically modified along margins and intra-clast pseudotachylite injections. The chemical modifications are extensive in smaller clasts \u003c5 μm diameter. At least three chemically distinct layers and domains in the pseudotachylite, and their fine-grained matrices, plot in sharply defined, well-segregated and non-overlapping fields in FeO + MgO−Al2O3–SiO2, FeO–CaO–MgO and CaO–Na2O–K2O and FeO vs. FeO/FeO + MgO diagrams. The compositions of the layers and domains—smeared between a feldspar + quartz component and a ferromagnesian component of garnet + Fe–Ti oxides (±orthopyroxene)—possibly correspond to fractionated quenched melts, or admixtures of microphenocrysts that cannot be resolved by the microbeam techniques employed. The compositional variations are incompatible with deformation-driven crystal fractionation in melt. Instead the layers and domains possibly are crystal-melt mushes produced by syn-deformation ultra-high temperature (1,250–1,375°C) melting reactions involving variable proportions of host-rock minerals determined by time-transient local phase aggregates experiencing strain. The similar element variation trends in pseudotachylite examined here and those reported from anorthosite, metapelite and charnockite elsewhere suggests local phase aggregate controlled multi-reaction melting is a phenomenon commoner than hitherto realized in pseudotachylites.","downloadable_attachments":[{"id":49129817,"asset_id":5808980,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":8522268,"first_name":"Naresh","last_name":"Pant","domain_name":"du-in","page_name":"NareshPant","display_name":"Naresh Pant","profile_url":"https://du-in.academia.edu/NareshPant?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":56001,"name":"X Rays","url":"https://www.academia.edu/Documents/in/X_Rays?f_ri=414","nofollow":false},{"id":1418721,"name":"Chemical Modification","url":"https://www.academia.edu/Documents/in/Chemical_Modification?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_71549897" data-work_id="71549897" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/71549897/MICROSCOPIA_DE_MENAS_ESTUDIO_Y_ANALISIS_DE">MICROSCOPIA DE MENAS – ESTUDIO Y ANALISIS DE</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/71549897" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="d86286ba93d0f1ad23d7ec2e18bde6f7" rel="nofollow" data-download="{"attachment_id":80844284,"asset_id":71549897,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/80844284/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="114545393" href="https://centrodeimagenysonido.academia.edu/KevenRomoGuzman">Keven Romo Guzman</a><script data-card-contents-for-user="114545393" type="text/json">{"id":114545393,"first_name":"Keven","last_name":"Romo Guzman","domain_name":"centrodeimagenysonido","page_name":"KevenRomoGuzman","display_name":"Keven Romo Guzman","profile_url":"https://centrodeimagenysonido.academia.edu/KevenRomoGuzman?f_ri=414","photo":"https://0.academia-photos.com/114545393/27589545/25916140/s65_keven.romo_guzman.jpg"}</script></span></span></li><li class="js-paper-rank-work_71549897 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="71549897"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 71549897, container: ".js-paper-rank-work_71549897", }); 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However, written or verbal tradition have given them a wide visibility and usage among both professionals and the general... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_45675993" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">There are a few trade names and expressions that are not exactly accurate if we look at them in a very strict way. However, written or verbal tradition have given them a wide visibility and usage among both professionals and the general public, and many have became part of the trade’s vernacular and nomenclature. Here are a few examples.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/45675993" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="3c9b9192154c15ab52ea6ba0e73ad437" rel="nofollow" data-download="{"attachment_id":74258858,"asset_id":45675993,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/74258858/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="131937289" href="https://independent.academia.edu/RuiGalopimdeCarvalho">Rui Galopim de Carvalho</a><script data-card-contents-for-user="131937289" type="text/json">{"id":131937289,"first_name":"Rui","last_name":"Galopim de Carvalho","domain_name":"independent","page_name":"RuiGalopimdeCarvalho","display_name":"Rui Galopim de Carvalho","profile_url":"https://independent.academia.edu/RuiGalopimdeCarvalho?f_ri=414","photo":"https://0.academia-photos.com/131937289/37974263/40899407/s65_rui.galopim_de_carvalho.png"}</script></span></span></li><li class="js-paper-rank-work_45675993 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="45675993"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 45675993, container: ".js-paper-rank-work_45675993", }); 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However, written or verbal tradition have given them a wide visibility and usage among both professionals and the general public, and many have became part of the trade’s vernacular and nomenclature. Here are a few examples.","downloadable_attachments":[{"id":74258858,"asset_id":45675993,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":131937289,"first_name":"Rui","last_name":"Galopim de Carvalho","domain_name":"independent","page_name":"RuiGalopimdeCarvalho","display_name":"Rui Galopim de Carvalho","profile_url":"https://independent.academia.edu/RuiGalopimdeCarvalho?f_ri=414","photo":"https://0.academia-photos.com/131937289/37974263/40899407/s65_rui.galopim_de_carvalho.png"}],"research_interests":[{"id":403,"name":"Gemology","url":"https://www.academia.edu/Documents/in/Gemology?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":5832,"name":"Terminology","url":"https://www.academia.edu/Documents/in/Terminology?f_ri=414","nofollow":false},{"id":65805,"name":"Nomenclature","url":"https://www.academia.edu/Documents/in/Nomenclature?f_ri=414","nofollow":false}]}, 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Dumanska-Słowik","profile_url":"https://independent.academia.edu/MagdalenaDumanskaS%C5%82owik?f_ri=414","photo":"https://0.academia-photos.com/6603007/23961707/22957173/s65_magdalena.dumanska-s_owik.jpg"}],"research_interests":[{"id":73,"name":"Civil Engineering","url":"https://www.academia.edu/Documents/in/Civil_Engineering?f_ri=414","nofollow":false},{"id":392,"name":"Archaeology","url":"https://www.academia.edu/Documents/in/Archaeology?f_ri=414","nofollow":false},{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=414"},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414"},{"id":2403,"name":"Environmental Geology","url":"https://www.academia.edu/Documents/in/Environmental_Geology?f_ri=414"},{"id":6825,"name":"RADIATION DAMAGE","url":"https://www.academia.edu/Documents/in/RADIATION_DAMAGE?f_ri=414"},{"id":21728,"name":"Clay Minerals","url":"https://www.academia.edu/Documents/in/Clay_Minerals?f_ri=414"},{"id":158165,"name":"Zinc","url":"https://www.academia.edu/Documents/in/Zinc?f_ri=414"},{"id":193878,"name":"Catena","url":"https://www.academia.edu/Documents/in/Catena?f_ri=414"},{"id":200896,"name":"Hydrothermal Alteration","url":"https://www.academia.edu/Documents/in/Hydrothermal_Alteration?f_ri=414"},{"id":217324,"name":"Soil sciences","url":"https://www.academia.edu/Documents/in/Soil_sciences?f_ri=414"},{"id":274263,"name":"Rare Earth Element Mineralization","url":"https://www.academia.edu/Documents/in/Rare_Earth_Element_Mineralization?f_ri=414"},{"id":299285,"name":"Mineral Composition","url":"https://www.academia.edu/Documents/in/Mineral_Composition?f_ri=414"},{"id":325160,"name":"Magma mixing","url":"https://www.academia.edu/Documents/in/Magma_mixing?f_ri=414"},{"id":525337,"name":"Explosive","url":"https://www.academia.edu/Documents/in/Explosive?f_ri=414"},{"id":554780,"name":"Interdisciplinary Engineering","url":"https://www.academia.edu/Documents/in/Interdisciplinary_Engineering?f_ri=414"},{"id":591410,"name":"Antarctic Peninsula","url":"https://www.academia.edu/Documents/in/Antarctic_Peninsula?f_ri=414"},{"id":709300,"name":"Trace element","url":"https://www.academia.edu/Documents/in/Trace_element?f_ri=414"},{"id":959838,"name":"Arabian Journal of Geosciences","url":"https://www.academia.edu/Documents/in/Arabian_Journal_of_Geosciences?f_ri=414"},{"id":1565116,"name":"Mixed layer","url":"https://www.academia.edu/Documents/in/Mixed_layer?f_ri=414"},{"id":1707373,"name":"Mass Balance","url":"https://www.academia.edu/Documents/in/Mass_Balance?f_ri=414"},{"id":1943986,"name":"Black Shale","url":"https://www.academia.edu/Documents/in/Black_Shale?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_10018224" data-work_id="10018224" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/10018224/Alkaline_rocks_and_carbonatites_of_Amba_Dongar_and_adjacent_areas_Deccan_Igneous_Province_Gujarat_India_1_Geology_petrography_and_petrochemistry">Alkaline rocks and carbonatites of Amba Dongar and adjacent areas, Deccan Igneous Province, Gujarat, India: 1. Geology, petrography and petrochemistry</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Rift-related, late Eocene (≈ 60 Ma) alkaline-carbonatitec intrusions cover ≈ 1200 km2 south of the town of Chhota Udaipur, and form a subprovince within the alkaline magmatism that accompanies the tholeiitic Deccan Traps. They were... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_10018224" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Rift-related, late Eocene (≈ 60 Ma) alkaline-carbonatitec intrusions cover ≈ 1200 km2 south of the town of Chhota Udaipur, and form a subprovince within the alkaline magmatism that accompanies the tholeiitic Deccan Traps. They were emplaced temporally between late Deccan Trap flows and late dykes of basalt and picritic basalt. The subprovince comprises five main geographic occurrences (sectors): (1)Amba Dongar: a ring-complex of Ca-Mg-Fe-carbonatites, nephelinites to tephriphonolites, and fluorite deposits; (2)Siriwasan-Dugdha: an intrusive complex of Ca—carbonatites, nephelinites and trachytic rocks; (3)Phenai Mata: a nepheline syenite plug and dykes, plus dykes of tephrites to phonolites and lamprophyres (intimately associated with a layered tholeiitic gabbro—granophyre intrusion); (4)Panwad-Kawant: dykes and plugs of lamprophyres and tephrites to phonolites; (5)Bakhatgarh-Phulmahal: late basic-ultrabasic dykes only. The alkaline rocks range from ultrasodic to ultrapotassic, but are mostly nonperalkaline. Silica-undersaturated examples show higher incompatible and LIL element contents (Rb, K, Nb, Zr, Sr, Ba, LREE, etc.) than the associated tholeiites. However, the late basic-ultrabasic dykes display an continuum of alkaline-tholeiitic compositions. Possible parent magmas are represented among the primitive undersaturated basic dykes (including lamprophyres). The trachytic rocks are subalkaline, and may be genetically related to a tholeiitic rather than alkaline parent magma. Alkalisch-karbonatitische Intrusionen aus dem Obereozän (≈60 Ma) erstrecken sich über 1200 km2 südlich der indischen Stadt Chhota Udaipur und bilden einen Teil des alkalischen Komplexes, der die tholeiitischen Deccan Traps begleitet. Die Gesteine wurden während eines Rifting Prozesses intrudiert und lagern stratigraphisch zwischen Deccan Trap Tholeiiten und basaltischen bzw. pikritischen Ganggesteinen. Das Gebiet läßt sich in fünf geographische Regionen unterteilen: (1) Amba Dongar: ein ringförmiger Komplex aus Ca-Mg-Fe-reichen Karbonatiten, Nepheliniten und Tephriphonoliten mit Fluorit-Lagerstätten; (2) Siriwasan-Dugdha: eine Ca-reiche Karbonatit-Intrusion mit Nepheliniten und Trachyten; (3) Phenai Mata: Eine Nephelin-syenitische Intrusion und begleitende Ganggesteine aus Tephriten, Phonoliten und Lamprophyren, die mit einer magmatisch geschichteten tholeiitischen Gabbro Intrusion vergesellschaftet sind; (4) Panwad-Kawant: Lamprophyrische Ganggesteine neben Tephriten und Phonoliten; (5) Bakhatgarh-Phulmahal: späte basisch bis ultrabasische Ganggesteine. Die alkalischen Gesteine besitzen eine ultrapotassische bis extrem Na-reiche Zusammensetzung, nur vereinzelte Proben weisen jedoch peralkalischen Charakter auf. Silizium-untersättigte (alkalische) Proben besitzen in der Regel höhere Konzentrationen an Mantel-inkompatiblen Elementen (z.B. LREE, Nb und Zr) und LILE (z.B. Rb, Sr und Ba) als die benachbarten Tholeiite. Die späten basisch bis ultrabasischen Ganggesteine stellen ein Kontinuum von alkalischer bis tholeiitischer Geochemie dar. Die “primitiven” Silizium-untersättigten Ganggesteine (und Lamprophyre) repräsentieren vermutlich die Ausgangssehmelzen; die “subalkalischen” Trachyte dürften in genetischem Zusammenhang mit den Tholeiiten stehen.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/10018224" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="ce96b62a0aa8afe8fe2df8788e8fb97f" rel="nofollow" data-download="{"attachment_id":47567908,"asset_id":10018224,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/47567908/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="24389812" href="https://unpsjb.academia.edu/santiagofernandez">santiago fernandez</a><script data-card-contents-for-user="24389812" type="text/json">{"id":24389812,"first_name":"santiago","last_name":"fernandez","domain_name":"unpsjb","page_name":"santiagofernandez","display_name":"santiago fernandez","profile_url":"https://unpsjb.academia.edu/santiagofernandez?f_ri=414","photo":"https://0.academia-photos.com/24389812/6580354/7439533/s65_santiago.fernandez.jpg_oh_842d585310a079d467c048201c67ba8d_oe_552c9067___gda___1429103431_8e63b7c643f227d0639574078642ab1e"}</script></span></span></li><li class="js-paper-rank-work_10018224 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="10018224"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 10018224, container: ".js-paper-rank-work_10018224", }); });</script></li><li class="js-percentile-work_10018224 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 10018224; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_10018224"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_10018224 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="10018224"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 10018224; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=10018224]").text(description); $(".js-view-count-work_10018224").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_10018224").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="10018224"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="517272" href="https://www.academia.edu/Documents/in/Mineralogy_and_Petrology">Mineralogy and Petrology</a><script data-card-contents-for-ri="517272" type="text/json">{"id":517272,"name":"Mineralogy and Petrology","url":"https://www.academia.edu/Documents/in/Mineralogy_and_Petrology?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=10018224]'), work: {"id":10018224,"title":"Alkaline rocks and carbonatites of Amba Dongar and adjacent areas, Deccan Igneous Province, Gujarat, India: 1. Geology, petrography and petrochemistry","created_at":"2015-01-05T10:22:36.867-08:00","url":"https://www.academia.edu/10018224/Alkaline_rocks_and_carbonatites_of_Amba_Dongar_and_adjacent_areas_Deccan_Igneous_Province_Gujarat_India_1_Geology_petrography_and_petrochemistry?f_ri=414","dom_id":"work_10018224","summary":"Rift-related, late Eocene (≈ 60 Ma) alkaline-carbonatitec intrusions cover ≈ 1200 km2 south of the town of Chhota Udaipur, and form a subprovince within the alkaline magmatism that accompanies the tholeiitic Deccan Traps. They were emplaced temporally between late Deccan Trap flows and late dykes of basalt and picritic basalt. The subprovince comprises five main geographic occurrences (sectors): (1)Amba Dongar: a ring-complex of Ca-Mg-Fe-carbonatites, nephelinites to tephriphonolites, and fluorite deposits; (2)Siriwasan-Dugdha: an intrusive complex of Ca—carbonatites, nephelinites and trachytic rocks; (3)Phenai Mata: a nepheline syenite plug and dykes, plus dykes of tephrites to phonolites and lamprophyres (intimately associated with a layered tholeiitic gabbro—granophyre intrusion); (4)Panwad-Kawant: dykes and plugs of lamprophyres and tephrites to phonolites; (5)Bakhatgarh-Phulmahal: late basic-ultrabasic dykes only. The alkaline rocks range from ultrasodic to ultrapotassic, but are mostly nonperalkaline. Silica-undersaturated examples show higher incompatible and LIL element contents (Rb, K, Nb, Zr, Sr, Ba, LREE, etc.) than the associated tholeiites. However, the late basic-ultrabasic dykes display an continuum of alkaline-tholeiitic compositions. Possible parent magmas are represented among the primitive undersaturated basic dykes (including lamprophyres). The trachytic rocks are subalkaline, and may be genetically related to a tholeiitic rather than alkaline parent magma. Alkalisch-karbonatitische Intrusionen aus dem Obereozän (≈60 Ma) erstrecken sich über 1200 km2 südlich der indischen Stadt Chhota Udaipur und bilden einen Teil des alkalischen Komplexes, der die tholeiitischen Deccan Traps begleitet. Die Gesteine wurden während eines Rifting Prozesses intrudiert und lagern stratigraphisch zwischen Deccan Trap Tholeiiten und basaltischen bzw. pikritischen Ganggesteinen. Das Gebiet läßt sich in fünf geographische Regionen unterteilen: (1) Amba Dongar: ein ringförmiger Komplex aus Ca-Mg-Fe-reichen Karbonatiten, Nepheliniten und Tephriphonoliten mit Fluorit-Lagerstätten; (2) Siriwasan-Dugdha: eine Ca-reiche Karbonatit-Intrusion mit Nepheliniten und Trachyten; (3) Phenai Mata: Eine Nephelin-syenitische Intrusion und begleitende Ganggesteine aus Tephriten, Phonoliten und Lamprophyren, die mit einer magmatisch geschichteten tholeiitischen Gabbro Intrusion vergesellschaftet sind; (4) Panwad-Kawant: Lamprophyrische Ganggesteine neben Tephriten und Phonoliten; (5) Bakhatgarh-Phulmahal: späte basisch bis ultrabasische Ganggesteine. Die alkalischen Gesteine besitzen eine ultrapotassische bis extrem Na-reiche Zusammensetzung, nur vereinzelte Proben weisen jedoch peralkalischen Charakter auf. Silizium-untersättigte (alkalische) Proben besitzen in der Regel höhere Konzentrationen an Mantel-inkompatiblen Elementen (z.B. LREE, Nb und Zr) und LILE (z.B. Rb, Sr und Ba) als die benachbarten Tholeiite. Die späten basisch bis ultrabasischen Ganggesteine stellen ein Kontinuum von alkalischer bis tholeiitischer Geochemie dar. Die “primitiven” Silizium-untersättigten Ganggesteine (und Lamprophyre) repräsentieren vermutlich die Ausgangssehmelzen; die “subalkalischen” Trachyte dürften in genetischem Zusammenhang mit den Tholeiiten stehen.","downloadable_attachments":[{"id":47567908,"asset_id":10018224,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":24389812,"first_name":"santiago","last_name":"fernandez","domain_name":"unpsjb","page_name":"santiagofernandez","display_name":"santiago fernandez","profile_url":"https://unpsjb.academia.edu/santiagofernandez?f_ri=414","photo":"https://0.academia-photos.com/24389812/6580354/7439533/s65_santiago.fernandez.jpg_oh_842d585310a079d467c048201c67ba8d_oe_552c9067___gda___1429103431_8e63b7c643f227d0639574078642ab1e"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":517272,"name":"Mineralogy and Petrology","url":"https://www.academia.edu/Documents/in/Mineralogy_and_Petrology?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_6731709" data-work_id="6731709" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/6731709/Kinetics_of_formation_of_zeolite_NaA_LTA_from_natural_kaolinites">Kinetics of formation of zeolite NaA [LTA] from natural kaolinites</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized"> The kinetics and mechanism of hydrothermal formation of zeolite A from natural kaolinites have been studied using as starting materials two international kaolinite standards (KGa-1 and KGa-2 from Georgia, USA) exhibiting a different... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_6731709" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden"> The kinetics and mechanism of hydrothermal formation of zeolite A from natural kaolinites have been studied using as starting materials two international kaolinite standards (KGa-1 and KGa-2 from Georgia, USA) exhibiting a different degree of stacking disorder. Precursors utilized for the synthesis were prepared by heating the kaolinites at 800 °C. Metakaolinite was also prepared from KGa-1 by thermal activation at 600 °C. The hydrothermal syntheses were accomplished by heating the samples in NaOH solutions at temperatures between 70 and 110 °C. The kinetic experiments were performed by time-resolved synchrotron powder diffraction in isothermal mode using a transmission geometry and an Image Plate detector. The results of the kinetic analysis are interpreted in the light of the structural state of the starting kaolinite, and of the temperature of activation of the precursor material. For kaolinite activated at high temperature the nucleation and crystallization of zeolite A is essentially independent of the defect density of the original kaolinite, and the thermal history of the precursor seems to be the main controlling parameter. The formation process of zeolite A from metakaolinite materials obtained at lower activation temperatures shows significantly faster reaction rates and lower apparent activation energies. This is again interpreted in the light of the short range inhomogeneities present in metakaolinite. As the reaction proceeds metastable zeolite A transforms into hydroxy-sodalite.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/6731709" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c609795a89c7916ff72276d8312faf64" rel="nofollow" data-download="{"attachment_id":48740606,"asset_id":6731709,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/48740606/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="1330562" href="https://unipd.academia.edu/GilbertoArtioli">Gilberto Artioli</a><script data-card-contents-for-user="1330562" type="text/json">{"id":1330562,"first_name":"Gilberto","last_name":"Artioli","domain_name":"unipd","page_name":"GilbertoArtioli","display_name":"Gilberto Artioli","profile_url":"https://unipd.academia.edu/GilbertoArtioli?f_ri=414","photo":"https://0.academia-photos.com/1330562/3274508/3853253/s65_gilberto.artioli.jpg"}</script></span></span></li><li class="js-paper-rank-work_6731709 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="6731709"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 6731709, container: ".js-paper-rank-work_6731709", }); });</script></li><li class="js-percentile-work_6731709 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 6731709; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_6731709"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_6731709 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="6731709"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 6731709; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=6731709]").text(description); $(".js-view-count-work_6731709").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_6731709").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="6731709"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="2157" href="https://www.academia.edu/Documents/in/Phase_Transformations">Phase Transformations</a>, <script data-card-contents-for-ri="2157" type="text/json">{"id":2157,"name":"Phase Transformations","url":"https://www.academia.edu/Documents/in/Phase_Transformations?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="43189" href="https://www.academia.edu/Documents/in/Chemical_Kinetics">Chemical Kinetics</a><script data-card-contents-for-ri="43189" type="text/json">{"id":43189,"name":"Chemical Kinetics","url":"https://www.academia.edu/Documents/in/Chemical_Kinetics?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=6731709]'), work: {"id":6731709,"title":"Kinetics of formation of zeolite NaA [LTA] from natural kaolinites","created_at":"2014-04-11T20:15:34.469-07:00","url":"https://www.academia.edu/6731709/Kinetics_of_formation_of_zeolite_NaA_LTA_from_natural_kaolinites?f_ri=414","dom_id":"work_6731709","summary":" The kinetics and mechanism of hydrothermal formation of zeolite A from natural kaolinites have been studied using as starting materials two international kaolinite standards (KGa-1 and KGa-2 from Georgia, USA) exhibiting a different degree of stacking disorder. Precursors utilized for the synthesis were prepared by heating the kaolinites at 800 °C. Metakaolinite was also prepared from KGa-1 by thermal activation at 600 °C. The hydrothermal syntheses were accomplished by heating the samples in NaOH solutions at temperatures between 70 and 110 °C. The kinetic experiments were performed by time-resolved synchrotron powder diffraction in isothermal mode using a transmission geometry and an Image Plate detector. The results of the kinetic analysis are interpreted in the light of the structural state of the starting kaolinite, and of the temperature of activation of the precursor material. For kaolinite activated at high temperature the nucleation and crystallization of zeolite A is essentially independent of the defect density of the original kaolinite, and the thermal history of the precursor seems to be the main controlling parameter. The formation process of zeolite A from metakaolinite materials obtained at lower activation temperatures shows significantly faster reaction rates and lower apparent activation energies. This is again interpreted in the light of the short range inhomogeneities present in metakaolinite. As the reaction proceeds metastable zeolite A transforms into hydroxy-sodalite.","downloadable_attachments":[{"id":48740606,"asset_id":6731709,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":1330562,"first_name":"Gilberto","last_name":"Artioli","domain_name":"unipd","page_name":"GilbertoArtioli","display_name":"Gilberto Artioli","profile_url":"https://unipd.academia.edu/GilbertoArtioli?f_ri=414","photo":"https://0.academia-photos.com/1330562/3274508/3853253/s65_gilberto.artioli.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":2157,"name":"Phase Transformations","url":"https://www.academia.edu/Documents/in/Phase_Transformations?f_ri=414","nofollow":false},{"id":43189,"name":"Chemical Kinetics","url":"https://www.academia.edu/Documents/in/Chemical_Kinetics?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_75816371" data-work_id="75816371" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/75816371/Geochemistry_and_tectonic_significance_of_the_Fannuj_Maskutan_SSZ_type_ophiolite_Inner_Makran_SE_Iran">Geochemistry and tectonic significance of the Fannuj-Maskutan SSZ-type ophiolite (Inner Makran, SE Iran</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up of lherzolites, harzburgites, layered... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_75816371" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up of lherzolites, harzburgites, layered and isotropic gabbros and diabase dikes and basaltic lavas. Here we present new textural description, mineral and whole-rock chemistry of peridotites together with bulk geochemistry of magmatic mafic rocks and U-Pb geochronology and Lu-Hf isotopes of inherited zircons in gabbros, with the aim to reconstruct the petrogenesis of the Fannuj-Maskutan ophiolite. The results indicate to a subduction-metasomatized depleted mantle source experienced 10-20% of partial melting. A transition from IAT-gabbros to E-MORB-basalts is also outlined. We interpret the obtained results as evidence for the Fannuj-Maskutan genesis in a supra-subduction zone (SSZ) basin developed in the Iranian cadomian crust as indicated by the presence of inherited Cadomian zircons (ca. 515 Ma, εHf (t) : −13.6-+11.2). Comparing the Fannuj-Maskutan ophiolites to well-known SSZ-systems such as the South Sandwich SSZ, and integrating with the existing literature on Inner Makran ophiolite belt we interpret the Fannuj-Maskutan ophiolite as a part of a major SSZ-basin opened in the Iranian cadomian crust and evolved during the Neotethys subduction under Central Iran.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/75816371" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="ada8aed6569d042295eb9547152f7ed8" rel="nofollow" data-download="{"attachment_id":83436503,"asset_id":75816371,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/83436503/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="40932563" href="https://kfs.academia.edu/DrMohamedKhedr">DrMohamed Khedr</a><script data-card-contents-for-user="40932563" type="text/json">{"id":40932563,"first_name":"DrMohamed","last_name":"Khedr","domain_name":"kfs","page_name":"DrMohamedKhedr","display_name":"DrMohamed Khedr","profile_url":"https://kfs.academia.edu/DrMohamedKhedr?f_ri=414","photo":"https://0.academia-photos.com/40932563/12744216/14174549/s65_drmohamed.khedr.jpg_oh_645cb2662ba11d040a88cc8044dc879c_oe_57e18c11"}</script></span></span></li><li class="js-paper-rank-work_75816371 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="75816371"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 75816371, container: ".js-paper-rank-work_75816371", }); 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$(".js-view-count[data-work-id=75816371]").text(description); $(".js-view-count-work_75816371").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_75816371").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="75816371"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">14</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="5218" href="https://www.academia.edu/Documents/in/Iranian_Studies">Iranian Studies</a>, <script data-card-contents-for-ri="5218" type="text/json">{"id":5218,"name":"Iranian Studies","url":"https://www.academia.edu/Documents/in/Iranian_Studies?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="7959" href="https://www.academia.edu/Documents/in/Stable_Isotope_Geochemistry">Stable Isotope Geochemistry</a>, <script data-card-contents-for-ri="7959" type="text/json">{"id":7959,"name":"Stable Isotope Geochemistry","url":"https://www.academia.edu/Documents/in/Stable_Isotope_Geochemistry?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="8116" href="https://www.academia.edu/Documents/in/Trace_element_Geochemistry">Trace element Geochemistry</a><script data-card-contents-for-ri="8116" type="text/json">{"id":8116,"name":"Trace element Geochemistry","url":"https://www.academia.edu/Documents/in/Trace_element_Geochemistry?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=75816371]'), work: {"id":75816371,"title":"Geochemistry and tectonic significance of the Fannuj-Maskutan SSZ-type ophiolite (Inner Makran, SE Iran","created_at":"2022-04-08T06:08:00.214-07:00","url":"https://www.academia.edu/75816371/Geochemistry_and_tectonic_significance_of_the_Fannuj_Maskutan_SSZ_type_ophiolite_Inner_Makran_SE_Iran?f_ri=414","dom_id":"work_75816371","summary":"The nature and geodynamic setting of Inner Makran ophiolites (SE Iran) are controversial and are the focus of a growing debate. The Fannuj-Maskutan ophiolite complex (central Inner Makran) is made up of lherzolites, harzburgites, layered and isotropic gabbros and diabase dikes and basaltic lavas. Here we present new textural description, mineral and whole-rock chemistry of peridotites together with bulk geochemistry of magmatic mafic rocks and U-Pb geochronology and Lu-Hf isotopes of inherited zircons in gabbros, with the aim to reconstruct the petrogenesis of the Fannuj-Maskutan ophiolite. The results indicate to a subduction-metasomatized depleted mantle source experienced 10-20% of partial melting. A transition from IAT-gabbros to E-MORB-basalts is also outlined. We interpret the obtained results as evidence for the Fannuj-Maskutan genesis in a supra-subduction zone (SSZ) basin developed in the Iranian cadomian crust as indicated by the presence of inherited Cadomian zircons (ca. 515 Ma, εHf (t) : −13.6-+11.2). Comparing the Fannuj-Maskutan ophiolites to well-known SSZ-systems such as the South Sandwich SSZ, and integrating with the existing literature on Inner Makran ophiolite belt we interpret the Fannuj-Maskutan ophiolite as a part of a major SSZ-basin opened in the Iranian cadomian crust and evolved during the Neotethys subduction under Central Iran.","downloadable_attachments":[{"id":83436503,"asset_id":75816371,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":40932563,"first_name":"DrMohamed","last_name":"Khedr","domain_name":"kfs","page_name":"DrMohamedKhedr","display_name":"DrMohamed Khedr","profile_url":"https://kfs.academia.edu/DrMohamedKhedr?f_ri=414","photo":"https://0.academia-photos.com/40932563/12744216/14174549/s65_drmohamed.khedr.jpg_oh_645cb2662ba11d040a88cc8044dc879c_oe_57e18c11"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":5218,"name":"Iranian Studies","url":"https://www.academia.edu/Documents/in/Iranian_Studies?f_ri=414","nofollow":false},{"id":7959,"name":"Stable Isotope Geochemistry","url":"https://www.academia.edu/Documents/in/Stable_Isotope_Geochemistry?f_ri=414","nofollow":false},{"id":8116,"name":"Trace element Geochemistry","url":"https://www.academia.edu/Documents/in/Trace_element_Geochemistry?f_ri=414","nofollow":false},{"id":16248,"name":"Ophiolites","url":"https://www.academia.edu/Documents/in/Ophiolites?f_ri=414"},{"id":16937,"name":"Petrology and Geochemistry","url":"https://www.academia.edu/Documents/in/Petrology_and_Geochemistry?f_ri=414"},{"id":22595,"name":"Geochronology \u0026 isotope Geology","url":"https://www.academia.edu/Documents/in/Geochronology_and_isotope_Geology?f_ri=414"},{"id":83087,"name":"Isotopes","url":"https://www.academia.edu/Documents/in/Isotopes?f_ri=414"},{"id":294417,"name":"Formation of Suprasubduction Ophiolite","url":"https://www.academia.edu/Documents/in/Formation_of_Suprasubduction_Ophiolite?f_ri=414"},{"id":598483,"name":"Continental Flood Basalt","url":"https://www.academia.edu/Documents/in/Continental_Flood_Basalt?f_ri=414"},{"id":832891,"name":"Tethyan Ophiolite","url":"https://www.academia.edu/Documents/in/Tethyan_Ophiolite?f_ri=414"},{"id":1384649,"name":"Mid Ocean Ridge Basalts","url":"https://www.academia.edu/Documents/in/Mid_Ocean_Ridge_Basalts?f_ri=414"},{"id":1872402,"name":"Pyroxenes","url":"https://www.academia.edu/Documents/in/Pyroxenes?f_ri=414"},{"id":3287424,"name":"Pyroxene exsolution textures in abyssal lherzolites","url":"https://www.academia.edu/Documents/in/Pyroxene_exsolution_textures_in_abyssal_lherzolites?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_41907918" data-work_id="41907918" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/41907918/Vymazalov%C3%A1ite_Pd3Bi2S2_a_new_mineral_from_the_Norilsk_Talnakh_deposit_Krasnoyarskiy_region_Russia_2_3">Vymazalováite, Pd3Bi2S2 , a new mineral from the Noril'sk -Talnakh deposit, Krasnoyarskiy region, Russia 2 3</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Vymazalováite, Pd3Bi2S2 is a new platinum-group mineral discovered in the Komsomolsky mine of the Talnakh deposit, Noril’sk district, Russia. It forms small (from a few μm to 20–35 µm) inclusions or euhedral grains in intergrowths of... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_41907918" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Vymazalováite, Pd3Bi2S2 is a new platinum-group mineral discovered in the Komsomolsky mine of the Talnakh deposit, Noril’sk district, Russia. It forms small (from a few μm to 20–35 µm) inclusions or euhedral grains in intergrowths of polarite, sobolevskite, acanthite and unnamed (Pd,Ag)5BiS2 in aggregates (up to ~200 µm) in galena and rarely in chalcopyrite. It occurs with telargpalite, cooperite, braggite, vysotskite, sopcheite, stibiopalladinite, sobolevskite, moncheite, kotulskite, malyshevite, insizwaite, Au-bearing silver and the newly described mineral kravtsovite (PdAg2S) in association with pyrite, chalcopyrite and galena in vein-disseminated mineralization in skarn rocks. Synthetic vymazalováite is brittle; it has a metallic lustre and a grey streak. In plane-polarized reflected light, vymazalováite is creamy grey and appears slightly brownish against galena in the assemblage with chalcopyrite. It exhibits no internal reflections. Average reflectance values in air for natural and synthetic vymazalováite are (R natural, R synthetic in %) are: 46.35, 45.7 at 470 nm, 47.65, 47.45 at 546 nm, 48.5, 48.2 at 589 nm and 49.5, 49.0 at 650 nm. Seven electron probe micro-analyses of vymazalováite give an average composition: Pd 40.42, Bi 49.15, Ag 0.55, Pb 1.02, S 7.77 and Se 0.26, total 99.17 wt.%, corresponding to the empirical formula Pd3.05(Bi1.89Ag0.04Pb0.04)Σ1.97(S1.95Se0.03)Σ1.98 based on a total of 7 atoms per formula unit. The simplified formula is Pd3Bi2S2. The mineral is cubic, space group I213, with a = 8.3097(9) Å, V = 573.79(1) Å3 and Z = 4. The density calculated on the basis of the empirical formula and cell dimensions of synthetic vymazalováite is 9.25 g/cm3. The strongest lines in the powder X-ray diffraction pattern of synthetic vymazalováite [d in Å (I) (hkl)] are: 4.15(32)(200), 2.93(78)(220), 2.40(100)(220), 2.08(53)(400), 1.695(34)(422), 1.468(35)(440) and 1.252(31)(622). The structural identity of natural vymazalováite with synthetic Pd3Bi2S2 was confirmed by electron back-scatter diffraction measurements on the natural sample. This new mineral honours Dr Anna Vymazalová of the Czech Geological Survey, Prague.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/41907918" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="a4513858c4a999958b9d41d399666d9b" rel="nofollow" data-download="{"attachment_id":62034854,"asset_id":41907918,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/62034854/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="15400748" href="https://independent.academia.edu/KozlovV">Vladimir Kozlov</a><script data-card-contents-for-user="15400748" type="text/json">{"id":15400748,"first_name":"Vladimir","last_name":"Kozlov","domain_name":"independent","page_name":"KozlovV","display_name":"Vladimir Kozlov","profile_url":"https://independent.academia.edu/KozlovV?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_41907918 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="41907918"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 41907918, container: ".js-paper-rank-work_41907918", }); 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It forms small (from a few μm to 20–35 µm) inclusions or euhedral grains in intergrowths of polarite, sobolevskite, acanthite and unnamed (Pd,Ag)5BiS2 in aggregates (up to ~200 µm) in galena and rarely in chalcopyrite. It occurs with telargpalite, cooperite, braggite, vysotskite, sopcheite, stibiopalladinite, sobolevskite, moncheite, kotulskite, malyshevite, insizwaite, Au-bearing silver and the newly described mineral kravtsovite (PdAg2S) in association with pyrite, chalcopyrite and galena in vein-disseminated mineralization in skarn rocks. Synthetic vymazalováite is brittle; it has a metallic lustre and a grey streak. In plane-polarized reflected light, vymazalováite is creamy grey and appears slightly brownish against galena in the assemblage with chalcopyrite. It exhibits no internal reflections. Average reflectance values in air for natural and synthetic vymazalováite are (R natural, R synthetic in %) are: 46.35, 45.7 at 470 nm, 47.65, 47.45 at 546 nm, 48.5, 48.2 at 589 nm and 49.5, 49.0 at 650 nm. Seven electron probe micro-analyses of vymazalováite give an average composition: Pd 40.42, Bi 49.15, Ag 0.55, Pb 1.02, S 7.77 and Se 0.26, total 99.17 wt.%, corresponding to the empirical formula Pd3.05(Bi1.89Ag0.04Pb0.04)Σ1.97(S1.95Se0.03)Σ1.98 based on a total of 7 atoms per formula unit. The simplified formula is Pd3Bi2S2. The mineral is cubic, space group I213, with a = 8.3097(9) Å, V = 573.79(1) Å3 and Z = 4. The density calculated on the basis of the empirical formula and cell dimensions of synthetic vymazalováite is 9.25 g/cm3. The strongest lines in the powder X-ray diffraction pattern of synthetic vymazalováite [d in Å (I) (hkl)] are: 4.15(32)(200), 2.93(78)(220), 2.40(100)(220), 2.08(53)(400), 1.695(34)(422), 1.468(35)(440) and 1.252(31)(622). The structural identity of natural vymazalováite with synthetic Pd3Bi2S2 was confirmed by electron back-scatter diffraction measurements on the natural sample. This new mineral honours Dr Anna Vymazalová of the Czech Geological Survey, Prague.","downloadable_attachments":[{"id":62034854,"asset_id":41907918,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":15400748,"first_name":"Vladimir","last_name":"Kozlov","domain_name":"independent","page_name":"KozlovV","display_name":"Vladimir Kozlov","profile_url":"https://independent.academia.edu/KozlovV?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":46378,"name":"Ore Geology","url":"https://www.academia.edu/Documents/in/Ore_Geology?f_ri=414","nofollow":false},{"id":201716,"name":"Palladium","url":"https://www.academia.edu/Documents/in/Palladium?f_ri=414","nofollow":false},{"id":895636,"name":"Massive Sulphide","url":"https://www.academia.edu/Documents/in/Massive_Sulphide?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_6731722" data-work_id="6731722" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/6731722/Kinetic_study_of_the_dehydroxylation_of_chrysotile_asbestos_with_temperature_by_in_situ_XRPD">Kinetic study of the dehydroxylation of chrysotile asbestos with temperature by in situ XRPD</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized"> The kinetics of the dehydroxylation of chrysotile was followed in situ at high temperature using real-time conventional and synchrotron powder diffraction (XRPD). This is the first time kinetics parameters have been calculated for the... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_6731722" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden"> The kinetics of the dehydroxylation of chrysotile was followed in situ at high temperature using real-time conventional and synchrotron powder diffraction (XRPD). This is the first time kinetics parameters have been calculated for the dehydroxylation of chrysotile. The value of the order of the reaction mechanism calculated using the Avrami model indicates that the rate-limiting step of the reaction is a one-dimensional diffusion with an instantaneous nucleation or a deceleratory rate of nucleation of the reaction product. Hence, the rate-limiting step is the one-dimensional diffusion of the water molecules formed in the interlayer region by direct condensation of two hydrogen atoms and an oxygen atom. The calculated apparent activation energy of the reaction in the temperature range 620–750 °C is 184 kJ mol−1. The diffusion path is along the axis of the fibrils forming the fibers. The amorphous or short-range ordered dehydroxylate of chrysotile is extremely unstable because forsterite readily nucleates in the Mg-rich regions. Moreover, it is less stable than the dehydroxylate of kaolinite, the so-called metakaolinite, which forms mullite at about 950 °C. This difference is interpreted in terms of the different nature of the two ions Mg2+ and Al3+ and their function as glass modifier and glass-forming ion, respectively.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/6731722" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="05da41400a16d0735ab5065cc96e2b2e" rel="nofollow" data-download="{"attachment_id":48740620,"asset_id":6731722,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/48740620/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="1330562" href="https://unipd.academia.edu/GilbertoArtioli">Gilberto Artioli</a><script data-card-contents-for-user="1330562" type="text/json">{"id":1330562,"first_name":"Gilberto","last_name":"Artioli","domain_name":"unipd","page_name":"GilbertoArtioli","display_name":"Gilberto Artioli","profile_url":"https://unipd.academia.edu/GilbertoArtioli?f_ri=414","photo":"https://0.academia-photos.com/1330562/3274508/3853253/s65_gilberto.artioli.jpg"}</script></span></span></li><li class="js-paper-rank-work_6731722 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="6731722"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 6731722, container: ".js-paper-rank-work_6731722", }); 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$(".js-view-count[data-work-id=6731722]").text(description); $(".js-view-count-work_6731722").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_6731722").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="6731722"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1177" href="https://www.academia.edu/Documents/in/Crystallography">Crystallography</a>, <script data-card-contents-for-ri="1177" type="text/json">{"id":1177,"name":"Crystallography","url":"https://www.academia.edu/Documents/in/Crystallography?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="73920" href="https://www.academia.edu/Documents/in/Asbestos">Asbestos</a>, <script data-card-contents-for-ri="73920" type="text/json">{"id":73920,"name":"Asbestos","url":"https://www.academia.edu/Documents/in/Asbestos?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="198733" href="https://www.academia.edu/Documents/in/Powder_X-Ray_Diffraction">Powder X-Ray Diffraction</a><script data-card-contents-for-ri="198733" type="text/json">{"id":198733,"name":"Powder X-Ray Diffraction","url":"https://www.academia.edu/Documents/in/Powder_X-Ray_Diffraction?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=6731722]'), work: {"id":6731722,"title":"Kinetic study of the dehydroxylation of chrysotile asbestos with temperature by in situ XRPD","created_at":"2014-04-11T20:16:02.911-07:00","url":"https://www.academia.edu/6731722/Kinetic_study_of_the_dehydroxylation_of_chrysotile_asbestos_with_temperature_by_in_situ_XRPD?f_ri=414","dom_id":"work_6731722","summary":" The kinetics of the dehydroxylation of chrysotile was followed in situ at high temperature using real-time conventional and synchrotron powder diffraction (XRPD). This is the first time kinetics parameters have been calculated for the dehydroxylation of chrysotile. The value of the order of the reaction mechanism calculated using the Avrami model indicates that the rate-limiting step of the reaction is a one-dimensional diffusion with an instantaneous nucleation or a deceleratory rate of nucleation of the reaction product. Hence, the rate-limiting step is the one-dimensional diffusion of the water molecules formed in the interlayer region by direct condensation of two hydrogen atoms and an oxygen atom. The calculated apparent activation energy of the reaction in the temperature range 620–750 °C is 184 kJ mol−1. The diffusion path is along the axis of the fibrils forming the fibers. The amorphous or short-range ordered dehydroxylate of chrysotile is extremely unstable because forsterite readily nucleates in the Mg-rich regions. Moreover, it is less stable than the dehydroxylate of kaolinite, the so-called metakaolinite, which forms mullite at about 950 °C. This difference is interpreted in terms of the different nature of the two ions Mg2+ and Al3+ and their function as glass modifier and glass-forming ion, respectively.","downloadable_attachments":[{"id":48740620,"asset_id":6731722,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":1330562,"first_name":"Gilberto","last_name":"Artioli","domain_name":"unipd","page_name":"GilbertoArtioli","display_name":"Gilberto Artioli","profile_url":"https://unipd.academia.edu/GilbertoArtioli?f_ri=414","photo":"https://0.academia-photos.com/1330562/3274508/3853253/s65_gilberto.artioli.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":1177,"name":"Crystallography","url":"https://www.academia.edu/Documents/in/Crystallography?f_ri=414","nofollow":false},{"id":73920,"name":"Asbestos","url":"https://www.academia.edu/Documents/in/Asbestos?f_ri=414","nofollow":false},{"id":198733,"name":"Powder X-Ray Diffraction","url":"https://www.academia.edu/Documents/in/Powder_X-Ray_Diffraction?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_59344445" data-work_id="59344445" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/59344445/Platinum_group_minerals_in_chromitites_from_the_ojen_lherzolite_massif_Serrania_de_Ronda_Betic_Cordillera_Southern_Spain_">Platinum-group minerals in chromitites from the ojen lherzolite massif (Serrania de Ronda, Betic Cordillera, Southern Spain)</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/59344445" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="912b5c41dd02656cafbb2fe37145925a" rel="nofollow" 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colouration of limnosilicites from the occurrence Banské (Slanské vrchy Mts., Eastern Slovakia)</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/2780894" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="dbf450b4b08b614852e3946bed199f6e" rel="nofollow" data-download="{"attachment_id":30753791,"asset_id":2780894,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" 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style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="2780894"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="9533" href="https://www.academia.edu/Documents/in/Minerals">Minerals</a>, <script data-card-contents-for-ri="9533" type="text/json">{"id":9533,"name":"Minerals","url":"https://www.academia.edu/Documents/in/Minerals?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="16023" href="https://www.academia.edu/Documents/in/Mineral_Chemistry">Mineral Chemistry</a><script data-card-contents-for-ri="16023" type="text/json">{"id":16023,"name":"Mineral Chemistry","url":"https://www.academia.edu/Documents/in/Mineral_Chemistry?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=2780894]'), work: {"id":2780894,"title":"Causes of colouration of limnosilicites from the occurrence Banské (Slanské vrchy Mts., Eastern 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Chemistry","url":"https://www.academia.edu/Documents/in/Mineral_Chemistry?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_29139260" data-work_id="29139260" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/29139260/Ngo_Thi_Huong_et_al_2016_Mineralogical_characteristics_of_arsenopyrite_and_pyrite_at_Bo_Va_and_Nam_Quang_gold_sulfide_deposits_Northeast_Vietnam_In_Vietnamese_VJES_38_1_">Ngo Thi Huong et al, 2016. Mineralogical characteristics of arsenopyrite and pyrite at Bo Va and Nam Quang gold-sulfide deposits (Northeast Vietnam) (In Vietnamese). VJES 38 (1)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Crystal morphology and chemical compositions of arsenopyrite and pyrite at the Nam Quang and Bo Va deposits in the Song Hien basin (Northeast Vietnam) are studied in detail. Arsenopyrite often forms elongated crystals. Their chemical... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_29139260" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Crystal morphology and chemical compositions of arsenopyrite and pyrite at the Nam Quang and Bo Va deposits in the Song <br />Hien basin (Northeast Vietnam) are studied in detail. Arsenopyrite often forms elongated crystals. Their chemical compositions are<br />relatively poor in As, but rich in S with S/As ratios often >1.1, impurity elements such as Ni, Co, Sb, and sometimes Au (up to 0.02<br />wt.%). Composition of the pyrite is stoichiometric, but with relatively high arsenic and (sometimes) gold. The correlation between<br />As and Au concentration in pyrite has been recorded. The morphology and chemical composition of arsenopyrite and pyrite of <br />Bo Va and Nam Quang deposits can be comparable to those in the Au-sulfide deposits in black shale in Kazakhstan and<br />Southeastern China.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/29139260" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="03d166b7ab4221323c853b3632ae8470" rel="nofollow" data-download="{"attachment_id":49586652,"asset_id":29139260,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/49586652/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="51980703" href="https://independent.academia.edu/VietnamJournalofEarthSciences">Vietnam Journal of Earth Sciences</a><script data-card-contents-for-user="51980703" type="text/json">{"id":51980703,"first_name":"Vietnam Journal of","last_name":"Earth Sciences","domain_name":"independent","page_name":"VietnamJournalofEarthSciences","display_name":"Vietnam Journal of Earth Sciences","profile_url":"https://independent.academia.edu/VietnamJournalofEarthSciences?f_ri=414","photo":"https://0.academia-photos.com/51980703/13756054/14867931/s65_vietnam_journal_of.earth_sciences.gif"}</script></span></span></li><li class="js-paper-rank-work_29139260 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="29139260"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 29139260, container: ".js-paper-rank-work_29139260", }); 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Mineralogical characteristics of arsenopyrite and pyrite at Bo Va and Nam Quang gold-sulfide deposits (Northeast Vietnam) (In Vietnamese). VJES 38 (1)","created_at":"2016-10-13T20:23:07.097-07:00","url":"https://www.academia.edu/29139260/Ngo_Thi_Huong_et_al_2016_Mineralogical_characteristics_of_arsenopyrite_and_pyrite_at_Bo_Va_and_Nam_Quang_gold_sulfide_deposits_Northeast_Vietnam_In_Vietnamese_VJES_38_1_?f_ri=414","dom_id":"work_29139260","summary":"Crystal morphology and chemical compositions of arsenopyrite and pyrite at the Nam Quang and Bo Va deposits in the Song \nHien basin (Northeast Vietnam) are studied in detail. Arsenopyrite often forms elongated crystals. Their chemical compositions are\nrelatively poor in As, but rich in S with S/As ratios often \u003e1.1, impurity elements such as Ni, Co, Sb, and sometimes Au (up to 0.02\nwt.%). Composition of the pyrite is stoichiometric, but with relatively high arsenic and (sometimes) gold. The correlation between\nAs and Au concentration in pyrite has been recorded. The morphology and chemical composition of arsenopyrite and pyrite of \nBo Va and Nam Quang deposits can be comparable to those in the Au-sulfide deposits in black shale in Kazakhstan and\nSoutheastern China.","downloadable_attachments":[{"id":49586652,"asset_id":29139260,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":51980703,"first_name":"Vietnam Journal of","last_name":"Earth Sciences","domain_name":"independent","page_name":"VietnamJournalofEarthSciences","display_name":"Vietnam Journal of Earth Sciences","profile_url":"https://independent.academia.edu/VietnamJournalofEarthSciences?f_ri=414","photo":"https://0.academia-photos.com/51980703/13756054/14867931/s65_vietnam_journal_of.earth_sciences.gif"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":6227,"name":"Arsenic","url":"https://www.academia.edu/Documents/in/Arsenic?f_ri=414","nofollow":false}]}, }) } 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$('*[data-has-card-for-ri-list=485542]'), work: {"id":485542,"title":"Pyrite deformation textures in the massive sulfide ore deposits of the Norwegian Caledonides","created_at":"2011-03-22T09:51:59.350-07:00","url":"https://www.academia.edu/485542/Pyrite_deformation_textures_in_the_massive_sulfide_ore_deposits_of_the_Norwegian_Caledonides?f_ri=414","dom_id":"work_485542","summary":null,"downloadable_attachments":[{"id":2212929,"asset_id":485542,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":117599,"first_name":"Alan","last_name":"Boyle","domain_name":"liverpool","page_name":"AlanBoyle","display_name":"Alan P Boyle","profile_url":"https://liverpool.academia.edu/AlanBoyle?f_ri=414","photo":"https://0.academia-photos.com/117599/31600/10439795/s65_alan.boyle.jpg"},{"id":33102417,"first_name":"Nigel","last_name":"Cook","domain_name":"adelaide1","page_name":"NigelCook","display_name":"Nigel 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class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/485538/An_analysis_of_the_microstructures_developed_in_experimentally_deformed_polycrystalline_pyrite_and_minor_sulphide_phases_using_electron_backscatter_diffraction">An analysis of the microstructures developed in experimentally deformed polycrystalline pyrite and minor sulphide phases using electron backscatter diffraction</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/485538" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="26a9e335790f4f94136426d0fc6a0dad" rel="nofollow" data-download="{"attachment_id":2212954,"asset_id":485538,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/2212954/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="117599" href="https://liverpool.academia.edu/AlanBoyle">Alan P Boyle</a><script data-card-contents-for-user="117599" 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$(".js-view-count-work_485538").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="485538"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">3</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="1419" href="https://www.academia.edu/Documents/in/Structural_Geology">Structural Geology</a>, <script data-card-contents-for-ri="1419" type="text/json">{"id":1419,"name":"Structural Geology","url":"https://www.academia.edu/Documents/in/Structural_Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="4237" href="https://www.academia.edu/Documents/in/Electron_Backscatter_Diffraction_EBSD_">Electron Backscatter Diffraction (EBSD)</a><script data-card-contents-for-ri="4237" type="text/json">{"id":4237,"name":"Electron Backscatter Diffraction (EBSD)","url":"https://www.academia.edu/Documents/in/Electron_Backscatter_Diffraction_EBSD_?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=485538]'), work: {"id":485538,"title":"An analysis of the microstructures developed in experimentally deformed polycrystalline pyrite and minor sulphide phases using electron backscatter 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Geology","url":"https://www.academia.edu/Documents/in/Structural_Geology?f_ri=414","nofollow":false},{"id":4237,"name":"Electron Backscatter Diffraction (EBSD)","url":"https://www.academia.edu/Documents/in/Electron_Backscatter_Diffraction_EBSD_?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_50819944" data-work_id="50819944" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/50819944/Les_mines_dantimoine_du_territoire_m%C3%A9tropolitain_de_la_prosp%C3%A9rit%C3%A9_%C3%A0_loubli">Les mines d'antimoine du territoire métropolitain, de la prospérité à l'oubli</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">La France a un riche passé minier pour l'antimoine. pierre-Christian Guiollard montre comment les mines du territoire métropolitain sont passées, du XVIe siècle à 1991, de la prospérité à l'oubli.</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/50819944" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="8aa9917e34bb35a5bbac23ecefc5fd73" rel="nofollow" data-download="{"attachment_id":68685965,"asset_id":50819944,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/68685965/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="125491847" href="https://independent.academia.edu/PierreGui2">Pierre-Christian GUIOLLARD</a><script data-card-contents-for-user="125491847" type="text/json">{"id":125491847,"first_name":"Pierre-Christian","last_name":"GUIOLLARD","domain_name":"independent","page_name":"PierreGui2","display_name":"Pierre-Christian GUIOLLARD","profile_url":"https://independent.academia.edu/PierreGui2?f_ri=414","photo":"https://0.academia-photos.com/125491847/45903195/35643246/s65_pierre.gui.jpg"}</script></span></span></li><li class="js-paper-rank-work_50819944 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="50819944"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 50819944, container: ".js-paper-rank-work_50819944", }); });</script></li><li class="js-percentile-work_50819944 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 50819944; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_50819944"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_50819944 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="50819944"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 50819944; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=50819944]").text(description); $(".js-view-count-work_50819944").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_50819944").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="50819944"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">9</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="14366" href="https://www.academia.edu/Documents/in/Mineral_Processing">Mineral Processing</a>, <script data-card-contents-for-ri="14366" type="text/json">{"id":14366,"name":"Mineral Processing","url":"https://www.academia.edu/Documents/in/Mineral_Processing?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="146671" href="https://www.academia.edu/Documents/in/Mineral_Resources">Mineral Resources</a><script data-card-contents-for-ri="146671" type="text/json">{"id":146671,"name":"Mineral Resources","url":"https://www.academia.edu/Documents/in/Mineral_Resources?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=50819944]'), work: {"id":50819944,"title":"Les mines d'antimoine du territoire métropolitain, de la prospérité à l'oubli","created_at":"2021-08-10T10:20:19.228-07:00","url":"https://www.academia.edu/50819944/Les_mines_dantimoine_du_territoire_m%C3%A9tropolitain_de_la_prosp%C3%A9rit%C3%A9_%C3%A0_loubli?f_ri=414","dom_id":"work_50819944","summary":"La France a un riche passé minier pour l'antimoine. pierre-Christian Guiollard montre comment les mines du territoire métropolitain sont passées, du XVIe siècle à 1991, de la prospérité à l'oubli.","downloadable_attachments":[{"id":68685965,"asset_id":50819944,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":125491847,"first_name":"Pierre-Christian","last_name":"GUIOLLARD","domain_name":"independent","page_name":"PierreGui2","display_name":"Pierre-Christian GUIOLLARD","profile_url":"https://independent.academia.edu/PierreGui2?f_ri=414","photo":"https://0.academia-photos.com/125491847/45903195/35643246/s65_pierre.gui.jpg"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":14366,"name":"Mineral Processing","url":"https://www.academia.edu/Documents/in/Mineral_Processing?f_ri=414","nofollow":false},{"id":146671,"name":"Mineral Resources","url":"https://www.academia.edu/Documents/in/Mineral_Resources?f_ri=414","nofollow":false},{"id":283848,"name":"Metallurgie","url":"https://www.academia.edu/Documents/in/Metallurgie?f_ri=414"},{"id":358012,"name":"Metallogeny","url":"https://www.academia.edu/Documents/in/Metallogeny?f_ri=414"},{"id":715662,"name":"Métallurgies Anciennes","url":"https://www.academia.edu/Documents/in/Metallurgies_Anciennes?f_ri=414"},{"id":1270382,"name":"Mines Et Métallurgie","url":"https://www.academia.edu/Documents/in/Mines_Et_Metallurgie?f_ri=414"},{"id":3709837,"name":"antimoine","url":"https://www.academia.edu/Documents/in/antimoine?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_37382128 coauthored" data-work_id="37382128" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/37382128/The_mineralogical_interpretation_of_particulate_matter_deposited_on_Agelenidae_and_Pholcidae_spider_webs_in_the_city_of_Wroc%C5%82aw_SW_Poland_A_preliminary_case_study">The mineralogical interpretation of particulate matter deposited on Agelenidae and Pholcidae spider webs in the city of Wrocław (SW Poland): A preliminary case study.</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The main goal of the study was to use SEM-EDX (Scanning Electron Microscope with Energy Dispersive X-Ray Analyser) for chemical and morphological characteristics of geological and trace elements particles identified on different types of... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_37382128" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The main goal of the study was to use SEM-EDX (Scanning Electron Microscope with Energy Dispersive X-Ray Analyser) for chemical and morphological characteristics of geological and trace elements particles identified on different types of webs (belonging to two different families of spiders) at various sampling locations in order to define the possible origin of deposited particulate matter. The research hypothesis assumes that particulate matter deriving from different polluted sites of Wroclaw agglomeration affects the structural properties of spider webs and on the basis of its mineralogical interpretation we can define the source of pollution. Spiders belonging to two families: Agelenidae and Pholcidae which are present in urban environment and weave relatively dense but structurally different webs have been chosen for studies as a potential passive bioindicators. Moreover, different time of spider web exposure was tested as a factor influenced final quality and quantity interpretation of data. Samples were collected from three sites in Wrocław city (SW Poland), all traffic-related. Two sites were close to each other with the same exposure time (40-days), the third one was localised in other part of the city and the web was exposed much longer (2-years). Additionally, silk obtained from the laboratory rearing of spiders was also examined (clean laboratory spider web) in relation to contaminated webs. The results reveal that geological and trace elements particles identified on two types of webs at neighbouring sites differ from each other as well as webs exposed to pollutants for longer time as a consequence of structural variation of webs and different exposure time. Pholcidae webs adsorber larger amounts of particles characterised by smaller diameter. Therefore, these webs are recommended as more perspective tool in contrast to Ageleniids webs which exhibit worse adsorption. The 1–2 month time of exposure of webs is adequate to quality and quantity interpretations of inorganic particles using SEM-EDX. Hence, we did not recommend longer exposure time due to possible alteration and secondary mineralogical artefact appearing. Our preliminary results indicated: (i) industry contribution is limited to gypsum and very sparse glass particles without metal-bearing particles derived from smelters localised on dominant wind direction, whereas the abundant mineral particles and carbon-rich particles derived probably from (ii) resuspension of local materials and fossil fuels combustion processes, suggesting super-local and local origin.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/37382128" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c8472b5ad576fb347cb72626241b5482" rel="nofollow" data-download="{"attachment_id":57344877,"asset_id":37382128,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/57344877/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="20806166" href="https://wroc.academia.edu/WojciechBartz">Wojciech Bartz</a><script data-card-contents-for-user="20806166" type="text/json">{"id":20806166,"first_name":"Wojciech","last_name":"Bartz","domain_name":"wroc","page_name":"WojciechBartz","display_name":"Wojciech Bartz","profile_url":"https://wroc.academia.edu/WojciechBartz?f_ri=414","photo":"https://0.academia-photos.com/20806166/5757896/11172654/s65_wojciech.bartz.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-37382128">+1</span><div class="hidden js-additional-users-37382128"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://pwr-wroc.academia.edu/JustynaRybak">Justyna Rybak</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-37382128'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-37382128').html(); 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container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_37382128 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="37382128"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 37382128; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=37382128]").text(description); $(".js-view-count-work_37382128").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_37382128").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="37382128"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">5</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="8738" href="https://www.academia.edu/Documents/in/Atmospheric_Aerosols">Atmospheric Aerosols</a>, <script data-card-contents-for-ri="8738" type="text/json">{"id":8738,"name":"Atmospheric Aerosols","url":"https://www.academia.edu/Documents/in/Atmospheric_Aerosols?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="10655" href="https://www.academia.edu/Documents/in/Scanning_Electron_Microscopy">Scanning Electron Microscopy</a>, <script data-card-contents-for-ri="10655" type="text/json">{"id":10655,"name":"Scanning Electron Microscopy","url":"https://www.academia.edu/Documents/in/Scanning_Electron_Microscopy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="11976" href="https://www.academia.edu/Documents/in/Air_pollution">Air pollution</a><script data-card-contents-for-ri="11976" type="text/json">{"id":11976,"name":"Air pollution","url":"https://www.academia.edu/Documents/in/Air_pollution?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=37382128]'), work: {"id":37382128,"title":"The mineralogical interpretation of particulate matter deposited on Agelenidae and Pholcidae spider webs in the city of Wrocław (SW Poland): A preliminary case study.","created_at":"2018-09-11T10:22:22.140-07:00","url":"https://www.academia.edu/37382128/The_mineralogical_interpretation_of_particulate_matter_deposited_on_Agelenidae_and_Pholcidae_spider_webs_in_the_city_of_Wroc%C5%82aw_SW_Poland_A_preliminary_case_study?f_ri=414","dom_id":"work_37382128","summary":"The main goal of the study was to use SEM-EDX (Scanning Electron Microscope with Energy Dispersive X-Ray Analyser) for chemical and morphological characteristics of geological and trace elements particles identified on different types of webs (belonging to two different families of spiders) at various sampling locations in order to define the possible origin of deposited particulate matter. The research hypothesis assumes that particulate matter deriving from different polluted sites of Wroclaw agglomeration affects the structural properties of spider webs and on the basis of its mineralogical interpretation we can define the source of pollution. Spiders belonging to two families: Agelenidae and Pholcidae which are present in urban environment and weave relatively dense but structurally different webs have been chosen for studies as a potential passive bioindicators. Moreover, different time of spider web exposure was tested as a factor influenced final quality and quantity interpretation of data. Samples were collected from three sites in Wrocław city (SW Poland), all traffic-related. Two sites were close to each other with the same exposure time (40-days), the third one was localised in other part of the city and the web was exposed much longer (2-years). Additionally, silk obtained from the laboratory rearing of spiders was also examined (clean laboratory spider web) in relation to contaminated webs. The results reveal that geological and trace elements particles identified on two types of webs at neighbouring sites differ from each other as well as webs exposed to pollutants for longer time as a consequence of structural variation of webs and different exposure time. Pholcidae webs adsorber larger amounts of particles characterised by smaller diameter. Therefore, these webs are recommended as more perspective tool in contrast to Ageleniids webs which exhibit worse adsorption. The 1–2 month time of exposure of webs is adequate to quality and quantity interpretations of inorganic particles using SEM-EDX. Hence, we did not recommend longer exposure time due to possible alteration and secondary mineralogical artefact appearing. Our preliminary results indicated: (i) industry contribution is limited to gypsum and very sparse glass particles without metal-bearing particles derived from smelters localised on dominant wind direction, whereas the abundant mineral particles and carbon-rich particles derived probably from (ii) resuspension of local materials and fossil fuels combustion processes, suggesting super-local and local origin.","downloadable_attachments":[{"id":57344877,"asset_id":37382128,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":20806166,"first_name":"Wojciech","last_name":"Bartz","domain_name":"wroc","page_name":"WojciechBartz","display_name":"Wojciech Bartz","profile_url":"https://wroc.academia.edu/WojciechBartz?f_ri=414","photo":"https://0.academia-photos.com/20806166/5757896/11172654/s65_wojciech.bartz.jpg"},{"id":35613561,"first_name":"Justyna","last_name":"Rybak","domain_name":"pwr-wroc","page_name":"JustynaRybak","display_name":"Justyna Rybak","profile_url":"https://pwr-wroc.academia.edu/JustynaRybak?f_ri=414","photo":"https://0.academia-photos.com/35613561/11778731/13129455/s65_justyna.rybak.jpg"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":8738,"name":"Atmospheric Aerosols","url":"https://www.academia.edu/Documents/in/Atmospheric_Aerosols?f_ri=414","nofollow":false},{"id":10655,"name":"Scanning Electron Microscopy","url":"https://www.academia.edu/Documents/in/Scanning_Electron_Microscopy?f_ri=414","nofollow":false},{"id":11976,"name":"Air pollution","url":"https://www.academia.edu/Documents/in/Air_pollution?f_ri=414","nofollow":false},{"id":25445,"name":"Environmental Pollution","url":"https://www.academia.edu/Documents/in/Environmental_Pollution?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_14130055" data-work_id="14130055" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/14130055/U_Pb_zircon_and_monazite_age_constraints_on_granulite_facies_metamorphism_and_deformation_in_the_Strangways_Metamorphic_Complex_central_Australia_">U–Pb zircon and monazite age constraints on granulite-facies metamorphism and deformation in the Strangways Metamorphic Complex (central Australia)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">... of the SMC. The granulite-facies rocks of the SMC are bounded by two major faults (Figs. 1 and 3), the Harry Creek Shear Zone to the South (Allen and Black 1979) and the Woo-langa Fault to the East. The SMC rock assemblage ...</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/14130055" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="4aef79104f8f9eb5f301ba47258b46fd" rel="nofollow" data-download="{"attachment_id":44604002,"asset_id":14130055,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/44604002/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="2538903" href="https://kansas.academia.edu/AndreasMoeller">Andreas Möller</a><script data-card-contents-for-user="2538903" type="text/json">{"id":2538903,"first_name":"Andreas","last_name":"Möller","domain_name":"kansas","page_name":"AndreasMoeller","display_name":"Andreas Möller","profile_url":"https://kansas.academia.edu/AndreasMoeller?f_ri=414","photo":"https://0.academia-photos.com/2538903/790901/982927/s65_andreas.moeller.jpg"}</script></span></span></li><li class="js-paper-rank-work_14130055 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="14130055"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 14130055, container: ".js-paper-rank-work_14130055", }); 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$(".js-view-count[data-work-id=14130055]").text(description); $(".js-view-count-work_14130055").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_14130055").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="14130055"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">4</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="407" href="https://www.academia.edu/Documents/in/Geochemistry">Geochemistry</a>, <script data-card-contents-for-ri="407" type="text/json">{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="191117" href="https://www.academia.edu/Documents/in/High_Temperature">High Temperature</a><script data-card-contents-for-ri="191117" type="text/json">{"id":191117,"name":"High Temperature","url":"https://www.academia.edu/Documents/in/High_Temperature?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=14130055]'), work: {"id":14130055,"title":"U–Pb zircon and monazite age constraints on granulite-facies metamorphism and deformation in the Strangways Metamorphic Complex (central Australia)","created_at":"2015-07-16T13:47:01.280-07:00","url":"https://www.academia.edu/14130055/U_Pb_zircon_and_monazite_age_constraints_on_granulite_facies_metamorphism_and_deformation_in_the_Strangways_Metamorphic_Complex_central_Australia_?f_ri=414","dom_id":"work_14130055","summary":"... of the SMC. The granulite-facies rocks of the SMC are bounded by two major faults (Figs. 1 and 3), the Harry Creek Shear Zone to the South (Allen and Black 1979) and the Woo-langa Fault to the East. The SMC rock assemblage ...","downloadable_attachments":[{"id":44604002,"asset_id":14130055,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":2538903,"first_name":"Andreas","last_name":"Möller","domain_name":"kansas","page_name":"AndreasMoeller","display_name":"Andreas Möller","profile_url":"https://kansas.academia.edu/AndreasMoeller?f_ri=414","photo":"https://0.academia-photos.com/2538903/790901/982927/s65_andreas.moeller.jpg"}],"research_interests":[{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":191117,"name":"High Temperature","url":"https://www.academia.edu/Documents/in/High_Temperature?f_ri=414","nofollow":false}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_9079474" data-work_id="9079474" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/9079474/Les_mines_de_Cerro_Minado_Hu%C3%A9rcal_Overa_Almer%C3%ADa_Espagne_Le_Cahier_des_micromonteurs_121_3_pp_3_122">Les mines de Cerro Minado, Huércal-Overa (Almería, Espagne), Le Cahier des micromonteurs 121 (3), pp. 3-122</a></div></div><div class="u-pb4x u-mt3x"></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/9079474" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa 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itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="386696" href="https://csic.academia.edu/NicolauEscanillaArtigas">Nicolau Escanilla Artigas</a><script data-card-contents-for-user="386696" type="text/json">{"id":386696,"first_name":"Nicolau","last_name":"Escanilla Artigas","domain_name":"csic","page_name":"NicolauEscanillaArtigas","display_name":"Nicolau Escanilla Artigas","profile_url":"https://csic.academia.edu/NicolauEscanillaArtigas?f_ri=414","photo":"https://0.academia-photos.com/386696/98029/36904975/s65_nicolau.escanilla_artigas.jpeg"}</script></span></span></li><li class="js-paper-rank-work_9079474 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="9079474"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 9079474, container: ".js-paper-rank-work_9079474", }); 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js-work-card work_51072925" data-work_id="51072925" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/51072925/Study_on_roof_tiles_colors_in_Malaysia_for_development_of_new_anti_warming_roof_tiles_with_higher_Solar_Reflectance_Index_SRI">Study on roof tile's colors in Malaysia for development of new anti-warming roof tiles with higher Solar Reflectance Index (SRI</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">This paper presents the preliminary findings of on going study intended to develop a cool house by introducing roofing materials with higher Solar Reflectance Index (SRI). SRI is a composed measure that accounts for surface&#x27;s solar... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_51072925" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">This paper presents the preliminary findings of on going study intended to develop a cool house by introducing roofing materials with higher Solar Reflectance Index (SRI). SRI is a composed measure that accounts for surface&#x27;s solar reflectance and emittance. It is ...</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/51072925" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="c98114b647e7ee6b623b5dc482895e9b" rel="nofollow" data-download="{"attachment_id":68928715,"asset_id":51072925,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/68928715/download_file?st=MTczMzMwNDQwNiw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="174165529" href="https://independent.academia.edu/SyedFarhan56">Syed Farhan</a><script data-card-contents-for-user="174165529" type="text/json">{"id":174165529,"first_name":"Syed","last_name":"Farhan","domain_name":"independent","page_name":"SyedFarhan56","display_name":"Syed Farhan","profile_url":"https://independent.academia.edu/SyedFarhan56?f_ri=414","photo":"/images/s65_no_pic.png"}</script></span></span></li><li class="js-paper-rank-work_51072925 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="51072925"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 51072925, container: ".js-paper-rank-work_51072925", }); 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SRI is a composed measure that accounts for surface\u0026#x27;s solar reflectance and emittance. It is ...","downloadable_attachments":[{"id":68928715,"asset_id":51072925,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":174165529,"first_name":"Syed","last_name":"Farhan","domain_name":"independent","page_name":"SyedFarhan56","display_name":"Syed Farhan","profile_url":"https://independent.academia.edu/SyedFarhan56?f_ri=414","photo":"/images/s65_no_pic.png"}],"research_interests":[{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":2065,"name":"Research Methodology","url":"https://www.academia.edu/Documents/in/Research_Methodology?f_ri=414","nofollow":false},{"id":4524,"name":"Sustainable Development","url":"https://www.academia.edu/Documents/in/Sustainable_Development?f_ri=414","nofollow":false},{"id":154596,"name":"Thermal comfort","url":"https://www.academia.edu/Documents/in/Thermal_comfort?f_ri=414","nofollow":false},{"id":234014,"name":"Thermal Performance","url":"https://www.academia.edu/Documents/in/Thermal_Performance?f_ri=414"},{"id":749302,"name":"Indexation","url":"https://www.academia.edu/Documents/in/Indexation?f_ri=414"},{"id":1457067,"name":"Questionnaire Survey","url":"https://www.academia.edu/Documents/in/Questionnaire_Survey?f_ri=414"},{"id":2556249,"name":"Postgraduate conference","url":"https://www.academia.edu/Documents/in/Postgraduate_conference?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_32268124" data-work_id="32268124" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/32268124/Strategic_and_rare_elements_in_Cretaceous_Cenozoic_cobalt_rich_ferromanganese_crusts_from_seamounts_in_the_Canary_Island_Seamount_Province_northeastern_tropical_Atlantic_">Strategic and rare elements in Cretaceous-Cenozoic cobalt-rich ferromanganese crusts from seamounts in the Canary Island Seamount Province (northeastern tropical Atlantic)</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">Thick ferromanganese (Fe-Mn) crusts from four Cretaceous seamounts (The Paps, Tropic, Echo and Drago) at the southern Canary Island Seamount Province (CISP) in the northeastern tropical Atlantic were recovered along the flanks and summits... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_32268124" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">Thick ferromanganese (Fe-Mn) crusts from four Cretaceous seamounts (The Paps, Tropic, Echo and Drago) at the southern Canary Island Seamount Province (CISP) in the northeastern tropical Atlantic were recovered along the flanks and summits from 1700 to 3000 m water depths. CISP is composed of N 100 seamounts and submarine hills, is likely the oldest hotspot track in the Atlantic Ocean, and is the most long-lived of known hotspots globally. The Fe-Mn crusts grow on basalt-sedimentary rock substrates below the northeastern tropical Atlantic core of the oxygen minimum zone (OMZ) with a maximum thickness of 250 mm at a water depth of 2400 m. The mineral-ogical and chemical composition of these Fe-Mn crusts indicate a hydrogenetic origin. The main Mn minerals are vernadite with minor interlayered todorokite and asbolane-buserite. Fe oxides are essentially ferroxyhyte and goethite. The Fe-Mn crusts show high average contents in Fe (23.5 wt%), Mn (16.1 wt%), and trace elements like Co (4700 μg/g), Ni (2800 μg/g), V (2400 μg/g) and Pb (1600 μg/g). Rare earth elements plus yttrium (REY) averages 2800 μg/g with high proportions of Ce (1600 μg/g). Total platinum group elements (PGEs) average 230 ng/g, with average Pt of 182 ng/g. Two main types of growth layers form the crusts: 1) a dense laminae of oxides with high contents in Mn, Co and Ni associated with vernadite and Cu, Ni, and Zn associated with todorokite; 2) botryoidal layers with high contents in Fe, Ti, V and REY associated with goethite. The Fe-Mn crusts from the CISP region show higher contents in Fe, V, Pb and REY but lower Mn, Co, Ni and PGEs contents than Pacific or Indian ocean seamount crusts. The oldest maximum age of initiation of crust growth was at 76 Ma (Cam-panian, Late Cretaceous). Using a combination of high resolution Co-chronometer and geochemical data along an Electron Probe Micro Analysis (EPMA) transect, four stages in morphology, chemical contents and growth rates can be differentiated in the the Cenozoic crusts since 28 Ma, which we interpret as due to changes in the ventilation of the North Atlantic OMZ and to the increase of Saharian dust inputs. An earliest growth period, characterized by similar contents of Fe and Mn in the interval 27.8–24.45 Ma (late Oligocene-early Miocene) reflects slow precipitation related to a thick OMZ. An intermediate laminated zone with higher contents of Fe, Si and P, high growth rates reaching 4.5 mm/Ma, and precipitation of Fe-Mn oxides during the interval 24.5–16 Ma is related to periods of ventilation of the OMZ by intrusion of deep upwelling currents. Significant increase in Fe contents at ca. 16 Ma correlates with the onset of incursions of Northern Component Waters into the North Atlantic. Finally, since 12 Ma, the very low growth rates (b0.5 mm/Ma) of the crust are related to a thick North Atlantic OMZ, an increase in Sahara dust input and a stable thermohaline circulation.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/32268124" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="01552b943d1a8269c6b43ed22543d381" rel="nofollow" data-download="{"attachment_id":52486882,"asset_id":32268124,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/52486882/download_file?st=MTczMzMwNDQwNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="783144" href="https://igme-es.academia.edu/FJavierGonz%C3%A1lezSanz">F. 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Javier González Sanz","profile_url":"https://igme-es.academia.edu/FJavierGonz%C3%A1lezSanz?f_ri=414","photo":"https://0.academia-photos.com/783144/266285/2414347/s65_f._javier.gonz_lez_sanz.jpg"}</script></span></span></li><li class="js-paper-rank-work_32268124 InlineList-item InlineList-item--bordered hidden"><span class="js-paper-rank-view hidden u-tcGrayDark" data-paper-rank-work-id="32268124"><i class="u-m1x fa fa-bar-chart"></i><strong class="js-paper-rank"></strong></span><script>$(function() { new Works.PaperRankView({ workId: 32268124, container: ".js-paper-rank-work_32268124", }); });</script></li><li class="js-percentile-work_32268124 InlineList-item InlineList-item--bordered hidden u-tcGrayDark"><span class="percentile-widget hidden"><span class="u-mr2x percentile-widget" style="display: none">•</span><span class="u-mr2x work-percentile"></span></span><script>$(function () { var workId = 32268124; window.Academia.workPercentilesFetcher.queue(workId, function (percentileText) { var container = $(".js-percentile-work_32268124"); container.find('.work-percentile').text(percentileText.charAt(0).toUpperCase() + percentileText.slice(1)); container.find('.percentile-widget').show(); container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_32268124 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="32268124"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 32268124; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=32268124]").text(description); $(".js-view-count-work_32268124").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_32268124").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="32268124"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">8</a>  </div><span class="InlineList-item-text u-textTruncate u-pl9x"><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="407" href="https://www.academia.edu/Documents/in/Geochemistry">Geochemistry</a>, <script data-card-contents-for-ri="407" type="text/json">{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="414" href="https://www.academia.edu/Documents/in/Mineralogy">Mineralogy</a>, <script data-card-contents-for-ri="414" type="text/json">{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="3110" href="https://www.academia.edu/Documents/in/Marine_Geology">Marine Geology</a><script data-card-contents-for-ri="3110" type="text/json">{"id":3110,"name":"Marine Geology","url":"https://www.academia.edu/Documents/in/Marine_Geology?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=32268124]'), work: {"id":32268124,"title":"Strategic and rare elements in Cretaceous-Cenozoic cobalt-rich ferromanganese crusts from seamounts in the Canary Island Seamount Province (northeastern tropical Atlantic)","created_at":"2017-04-05T03:17:04.435-07:00","url":"https://www.academia.edu/32268124/Strategic_and_rare_elements_in_Cretaceous_Cenozoic_cobalt_rich_ferromanganese_crusts_from_seamounts_in_the_Canary_Island_Seamount_Province_northeastern_tropical_Atlantic_?f_ri=414","dom_id":"work_32268124","summary":"Thick ferromanganese (Fe-Mn) crusts from four Cretaceous seamounts (The Paps, Tropic, Echo and Drago) at the southern Canary Island Seamount Province (CISP) in the northeastern tropical Atlantic were recovered along the flanks and summits from 1700 to 3000 m water depths. CISP is composed of N 100 seamounts and submarine hills, is likely the oldest hotspot track in the Atlantic Ocean, and is the most long-lived of known hotspots globally. The Fe-Mn crusts grow on basalt-sedimentary rock substrates below the northeastern tropical Atlantic core of the oxygen minimum zone (OMZ) with a maximum thickness of 250 mm at a water depth of 2400 m. The mineral-ogical and chemical composition of these Fe-Mn crusts indicate a hydrogenetic origin. The main Mn minerals are vernadite with minor interlayered todorokite and asbolane-buserite. Fe oxides are essentially ferroxyhyte and goethite. The Fe-Mn crusts show high average contents in Fe (23.5 wt%), Mn (16.1 wt%), and trace elements like Co (4700 μg/g), Ni (2800 μg/g), V (2400 μg/g) and Pb (1600 μg/g). Rare earth elements plus yttrium (REY) averages 2800 μg/g with high proportions of Ce (1600 μg/g). Total platinum group elements (PGEs) average 230 ng/g, with average Pt of 182 ng/g. Two main types of growth layers form the crusts: 1) a dense laminae of oxides with high contents in Mn, Co and Ni associated with vernadite and Cu, Ni, and Zn associated with todorokite; 2) botryoidal layers with high contents in Fe, Ti, V and REY associated with goethite. The Fe-Mn crusts from the CISP region show higher contents in Fe, V, Pb and REY but lower Mn, Co, Ni and PGEs contents than Pacific or Indian ocean seamount crusts. The oldest maximum age of initiation of crust growth was at 76 Ma (Cam-panian, Late Cretaceous). Using a combination of high resolution Co-chronometer and geochemical data along an Electron Probe Micro Analysis (EPMA) transect, four stages in morphology, chemical contents and growth rates can be differentiated in the the Cenozoic crusts since 28 Ma, which we interpret as due to changes in the ventilation of the North Atlantic OMZ and to the increase of Saharian dust inputs. An earliest growth period, characterized by similar contents of Fe and Mn in the interval 27.8–24.45 Ma (late Oligocene-early Miocene) reflects slow precipitation related to a thick OMZ. An intermediate laminated zone with higher contents of Fe, Si and P, high growth rates reaching 4.5 mm/Ma, and precipitation of Fe-Mn oxides during the interval 24.5–16 Ma is related to periods of ventilation of the OMZ by intrusion of deep upwelling currents. Significant increase in Fe contents at ca. 16 Ma correlates with the onset of incursions of Northern Component Waters into the North Atlantic. Finally, since 12 Ma, the very low growth rates (b0.5 mm/Ma) of the crust are related to a thick North Atlantic OMZ, an increase in Sahara dust input and a stable thermohaline circulation.","downloadable_attachments":[{"id":52486882,"asset_id":32268124,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":783144,"first_name":"F. Javier","last_name":"González Sanz","domain_name":"igme-es","page_name":"FJavierGonzálezSanz","display_name":"F. Javier González Sanz","profile_url":"https://igme-es.academia.edu/FJavierGonz%C3%A1lezSanz?f_ri=414","photo":"https://0.academia-photos.com/783144/266285/2414347/s65_f._javier.gonz_lez_sanz.jpg"}],"research_interests":[{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=414","nofollow":false},{"id":407,"name":"Geochemistry","url":"https://www.academia.edu/Documents/in/Geochemistry?f_ri=414","nofollow":false},{"id":414,"name":"Mineralogy","url":"https://www.academia.edu/Documents/in/Mineralogy?f_ri=414","nofollow":false},{"id":3110,"name":"Marine Geology","url":"https://www.academia.edu/Documents/in/Marine_Geology?f_ri=414","nofollow":false},{"id":4121,"name":"Atlantic World","url":"https://www.academia.edu/Documents/in/Atlantic_World?f_ri=414"},{"id":29057,"name":"Manganese","url":"https://www.academia.edu/Documents/in/Manganese?f_ri=414"},{"id":46378,"name":"Ore Geology","url":"https://www.academia.edu/Documents/in/Ore_Geology?f_ri=414"},{"id":140498,"name":"Seamounts","url":"https://www.academia.edu/Documents/in/Seamounts?f_ri=414"}]}, }) } })();</script></ul></li></ul></div></div><div class="u-borderBottom1 u-borderColorGrayLighter"><div class="clearfix u-pv7x u-mb0x js-work-card work_44518656" data-work_id="44518656" itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/44518656/CARACTERIZACI%C3%93N_TRIDIMENSIONAL_DE_LOS_MINERALES_MET%C3%81LICOS_PRESENTES_EN_LAS_CONDRITAS_ORDINARIAS">CARACTERIZACIÓN TRIDIMENSIONAL DE LOS MINERALES METÁLICOS PRESENTES EN LAS CONDRITAS ORDINARIAS</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">El presente trabajo tiene como objetivo caracterizar los minerales metálicos presentes en las condritas ordinarias relacionados con el resto de componentes minerales, y evaluar el uso de la microtomografía de rayos X como una herramienta... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_44518656" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">El presente trabajo tiene como objetivo caracterizar los minerales metálicos presentes en las condritas ordinarias relacionados con el resto de componentes minerales, y evaluar el uso de la microtomografía de rayos X como una herramienta para realizar estudios de distribución tridimensional, necesariamente integrada con una caracterización convencional mediante otras técnicas analíticas básicas. Para ello, se lleva a cabo una completa caracterización petrográfica de la condrita ordinaria KG007 (tipo H6), encontrada en el desierto del Sáhara. Dicha caracterización ha sido realizada a través de análisis petrográficos a diferentes escalas, utilizando las siguientes técnicas: 1) microscopía óptica polarizada de luz trasmitida y reflejada, 2) SEM-EDS, y 3) microtomografía de rayos X.<br /><br />Los meteoritos son fragmentos rocosos extraterrestres que contienen en su interior un registro exclusivo de la historia del Universo. Dada su procedencia, la disponibilidad de ejemplares de estos materiales, es escasa. Es por ello que, resulta importante abordar sus estudios bajo la premisa de una máxima conservación posible. En este trabajo se exponen algunas ideas sobre las metodologías de análisis mineral aplicadas al estudio de meteoritos y se hace especial énfasis en la técnica de microtomografía de rayos X, ya que representa la base de una nueva generación de equipos que permitirán el estudio cualitativo y cuantitativo de los meteoritos desde un marco tridimensional, sin que ello implique una destrucción total de la muestra.<br /><br />De los resultados obtenidos en este estudio, se infiere que la microtomografía de rayos X es una técnica idónea para la visualización tridimensional de los componentes minerales de los meteoritos y en especial, de la fase metálica, puesto que permite distinguir y determinar morfologías, distribución, abundancia modal y texturas, en contraste con las otras técnicas que sólo aportan información bidimensional. La información obtenida sobre estos minerales metálicos puede resultar valiosa sobre un amplio abanico de investigaciones enfocado a la reconstrucción de los cuerpos menores del espacio, como los asteroides, así como aspectos de las condiciones de formación del Sistema Solar.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/44518656" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="e9958d979368a3f7443067c819b79b60" rel="nofollow" data-download="{"attachment_id":64961135,"asset_id":44518656,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/64961135/download_file?st=MTczMzMwNDQwNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="177541521" href="https://viu-es.academia.edu/KellyGuiomarPadillaMontoya">Kelly G . Padilla Montoya</a><script data-card-contents-for-user="177541521" type="text/json">{"id":177541521,"first_name":"Kelly","last_name":"Padilla Montoya","domain_name":"viu-es","page_name":"KellyGuiomarPadillaMontoya","display_name":"Kelly G . 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Para ello, se lleva a cabo una completa caracterización petrográfica de la condrita ordinaria KG007 (tipo H6), encontrada en el desierto del Sáhara. Dicha caracterización ha sido realizada a través de análisis petrográficos a diferentes escalas, utilizando las siguientes técnicas: 1) microscopía óptica polarizada de luz trasmitida y reflejada, 2) SEM-EDS, y 3) microtomografía de rayos X.\n\nLos meteoritos son fragmentos rocosos extraterrestres que contienen en su interior un registro exclusivo de la historia del Universo. Dada su procedencia, la disponibilidad de ejemplares de estos materiales, es escasa. Es por ello que, resulta importante abordar sus estudios bajo la premisa de una máxima conservación posible. En este trabajo se exponen algunas ideas sobre las metodologías de análisis mineral aplicadas al estudio de meteoritos y se hace especial énfasis en la técnica de microtomografía de rayos X, ya que representa la base de una nueva generación de equipos que permitirán el estudio cualitativo y cuantitativo de los meteoritos desde un marco tridimensional, sin que ello implique una destrucción total de la muestra.\n\nDe los resultados obtenidos en este estudio, se infiere que la microtomografía de rayos X es una técnica idónea para la visualización tridimensional de los componentes minerales de los meteoritos y en especial, de la fase metálica, puesto que permite distinguir y determinar morfologías, distribución, abundancia modal y texturas, en contraste con las otras técnicas que sólo aportan información bidimensional. La información obtenida sobre estos minerales metálicos puede resultar valiosa sobre un amplio abanico de investigaciones enfocado a la reconstrucción de los cuerpos menores del espacio, como los asteroides, así como aspectos de las condiciones de formación del Sistema Solar.","downloadable_attachments":[{"id":64961135,"asset_id":44518656,"asset_type":"Work","always_allow_download":false}],"ordered_authors":[{"id":177541521,"first_name":"Kelly","last_name":"Padilla Montoya","domain_name":"viu-es","page_name":"KellyGuiomarPadillaMontoya","display_name":"Kelly G . 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href="https://www.academia.edu/41414287/expos%C3%A9_proc%C3%A9d%C3%A9s_minerale">exposé procédés minerale</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest">exposé sur le minerai de baryte</div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/41414287" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="42fdb2cb9a5d34ee976039421bcf9b51" rel="nofollow" data-download="{"attachment_id":61601130,"asset_id":41414287,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" 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itemscope="itemscope" itemtype="https://schema.org/ScholarlyArticle"><div class="header"><div class="title u-fontSerif u-fs22 u-lineHeight1_3"><a class="u-tcGrayDarkest js-work-link" href="https://www.academia.edu/3661207/The_Discovery_and_History_of_Dalgaranga_Meteorite_Crater_Western_Australia">The Discovery and History of Dalgaranga Meteorite Crater, Western Australia</a></div></div><div class="u-pb4x u-mt3x"><div class="summary u-fs14 u-fw300 u-lineHeight1_5 u-tcGrayDarkest"><div class="summarized">The Dalgaranga meteorite crater, 100 km northeast of Yalgoo, Western Australia, was the first impact structure identified in Australia, the smallest isolated crater found in Australia, and the only confirmed crater in the world associated... <a class="more_link u-tcGrayDark u-linkUnstyled" data-container=".work_3661207" data-show=".complete" data-hide=".summarized" data-more-link-behavior="true" href="#">more</a></div><div class="complete hidden">The Dalgaranga meteorite crater, 100 km northeast of Yalgoo, Western Australia, was the first impact structure identified in Australia, the smallest isolated crater found in Australia, and the only confirmed crater in the world associated with a mesosiderite projectile. 17 years passed before the Dalgaranga meteorites were described in the scientific literature and nearly 40 years passed before a survey of the structure was published. The reasons for the time-gap were never explained and a number of factual errors about the discovery and early history remain uncorrected in the scientific literature. Using historical and archival documents and accounts from people involved in early Dalgaranga research, we provide a detailed history of the discovery and study of the crater and its associated meteorites. We then discuss discrepancies in the age estimates of the impact and use pi-scaling laws to estimate the mass of the projectile.</div></div></div><ul class="InlineList u-ph0x u-fs13"><li class="InlineList-item logged_in_only"><div class="share_on_academia_work_button"><a class="academia_share Button Button--inverseBlue Button--sm js-bookmark-button" data-academia-share="Work/3661207" data-share-source="work_strip" data-spinner="small_white_hide_contents"><i class="fa fa-plus"></i><span class="work-strip-link-text u-ml1x" data-content="button_text">Bookmark</span></a></div></li><li class="InlineList-item"><div class="download"><a id="23549bf49ab44ab01be2021552d04db1" rel="nofollow" data-download="{"attachment_id":40990472,"asset_id":3661207,"asset_type":"Work","always_allow_download":false,"track":null,"button_location":"work_strip","source":null,"hide_modal":null}" class="Button Button--sm Button--inverseGreen js-download-button prompt_button doc_download" href="https://www.academia.edu/attachments/40990472/download_file?st=MTczMzMwNDQwNyw4LjIyMi4yMDguMTQ2&s=work_strip"><i class="fa fa-arrow-circle-o-down fa-lg"></i><span class="u-textUppercase u-ml1x" data-content="button_text">Download</span></a></div></li><li class="InlineList-item"><ul class="InlineList InlineList--bordered u-ph0x"><li class="InlineList-item InlineList-item--bordered"><span class="InlineList-item-text">by <span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a class="u-tcGrayDark u-fw700" data-has-card-for-user="6281699" href="https://mq.academia.edu/CONeill">Craig O'Neill</a><script data-card-contents-for-user="6281699" type="text/json">{"id":6281699,"first_name":"Craig","last_name":"O'Neill","domain_name":"mq","page_name":"CONeill","display_name":"Craig O'Neill","profile_url":"https://mq.academia.edu/CONeill?f_ri=414","photo":"https://0.academia-photos.com/6281699/43513061/34555654/s65_craig.o_neill.jpg"}</script></span></span><span class="u-displayInlineBlock InlineList-item-text"> and <span class="u-textDecorationUnderline u-clickable InlineList-item-text js-work-more-authors-3661207">+1</span><div class="hidden js-additional-users-3661207"><div><span itemscope="itemscope" itemprop="author" itemtype="https://schema.org/Person"><a href="https://unimelb.academia.edu/DuaneHamacher">Duane Hamacher</a></span></div></div></span><script>(function(){ var popoverSettings = { el: $('.js-work-more-authors-3661207'), placement: 'bottom', hide_delay: 200, html: true, content: function(){ return $('.js-additional-users-3661207').html(); 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container.find('.percentile-widget').removeClass('hidden'); }); });</script></li><li class="js-view-count-work_3661207 InlineList-item InlineList-item--bordered hidden"><div><span><span class="js-view-count view-count u-mr2x" data-work-id="3661207"><i class="fa fa-spinner fa-spin"></i></span><script>$(function () { var workId = 3661207; window.Academia.workViewCountsFetcher.queue(workId, function (count) { var description = window.$h.commaizeInt(count) + " " + window.$h.pluralize(count, 'View'); $(".js-view-count[data-work-id=3661207]").text(description); $(".js-view-count-work_3661207").attr('title', description).tooltip(); }); });</script></span><script>$(function() { $(".js-view-count-work_3661207").removeClass('hidden') })</script></div></li><li class="InlineList-item u-positionRelative" style="max-width: 250px"><div class="u-positionAbsolute" data-has-card-for-ri-list="3661207"><i class="fa fa-tag InlineList-item-icon u-positionRelative"></i>  <a class="InlineList-item-text u-positionRelative">30</a>  </div><span class="InlineList-item-text u-textTruncate u-pl10x"><a class="InlineList-item-text" data-has-card-for-ri="128" href="https://www.academia.edu/Documents/in/History">History</a>, <script data-card-contents-for-ri="128" type="text/json">{"id":128,"name":"History","url":"https://www.academia.edu/Documents/in/History?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="400" href="https://www.academia.edu/Documents/in/Earth_Sciences">Earth Sciences</a>, <script data-card-contents-for-ri="400" type="text/json">{"id":400,"name":"Earth Sciences","url":"https://www.academia.edu/Documents/in/Earth_Sciences?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="406" href="https://www.academia.edu/Documents/in/Geology">Geology</a>, <script data-card-contents-for-ri="406" type="text/json">{"id":406,"name":"Geology","url":"https://www.academia.edu/Documents/in/Geology?f_ri=414","nofollow":false}</script><a class="InlineList-item-text" data-has-card-for-ri="409" href="https://www.academia.edu/Documents/in/Geophysics">Geophysics</a><script data-card-contents-for-ri="409" type="text/json">{"id":409,"name":"Geophysics","url":"https://www.academia.edu/Documents/in/Geophysics?f_ri=414","nofollow":false}</script></span></li><script>(function(){ if (true) { new Aedu.ResearchInterestListCard({ el: $('*[data-has-card-for-ri-list=3661207]'), work: {"id":3661207,"title":"The Discovery and History of Dalgaranga Meteorite Crater, Western Australia","created_at":"2013-06-05T18:59:17.713-07:00","url":"https://www.academia.edu/3661207/The_Discovery_and_History_of_Dalgaranga_Meteorite_Crater_Western_Australia?f_ri=414","dom_id":"work_3661207","summary":"The Dalgaranga meteorite crater, 100 km northeast of Yalgoo, Western Australia, was the first impact structure identified in Australia, the smallest isolated crater found in Australia, and the only confirmed crater in the world associated with a mesosiderite projectile. 17 years passed before the Dalgaranga meteorites were described in the scientific literature and nearly 40 years passed before a survey of the structure was published. The reasons for the time-gap were never explained and a number of factual errors about the discovery and early history remain uncorrected in the scientific literature. Using historical and archival documents and accounts from people involved in early Dalgaranga research, we provide a detailed history of the discovery and study of the crater and its associated meteorites. 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