SE - Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments

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href="https://cdn.copernicus.org/libraries/photoswipe/4.1/dark-icon-skin/dark-icon-skin.css"> <base href="/"> <link rel="stylesheet" type="text/css" href="https://cdn.copernicus.org/libraries/unsemantic/unsemantic.min.css"> <link rel="stylesheet" type="text/css" href="https://cdn.copernicus.org/libraries/jquery/1.11.1/ui/jquery-ui.min.css"> <link rel="stylesheet" type="text/css" href="https://cdn.copernicus.org/libraries/jquery/1.11.1/ui/jquery-ui-slider-pips.css"> <link rel="stylesheet" type="text/css" href="https://cdn.copernicus.org/libraries/photoswipe/4.1/photoswipe.css"> <link rel="stylesheet" type="text/css" href="https://cdn.copernicus.org/apps/htmlgenerator/css/htmlgenerator.css?v=1"> <meta name="citation_fulltext_world_readable" content=""> <meta name="citation_publisher" content="Copernicus GmbH"/> <meta name="citation_title" content="Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments"/> <meta name="citation_abstract" content="<p><strong class="journal-contentHeaderColor">Abstract.</strong> Allochthonous accreted terranes are exotic geologic units that originated from anomalous crustal regions on a subducting oceanic plate and were transferred to the overriding plate by accretionary processes during subduction. The geographical regions that eventually become accreted allochthonous terranes include island arcs, oceanic plateaus, submarine ridges, seamounts, continental fragments, and microcontinents. These future allochthonous terranes (FATs) contribute to continental crustal growth, subduction dynamics, and crustal recycling in the mantle. We present a review of modern FATs and their accreted counterparts based on available geological, seismic, and gravity studies and discuss their crustal structure, geological origin, and bulk crustal density. Island arcs have an average crustal thickness of 26 km, average bulk crustal density of 2.79 g cm<sup>−3</sup>, and three distinct crustal units overlying a crust–mantle transition zone. Oceanic plateaus and submarine ridges have an average crustal thickness of 21 km and average bulk crustal density of 2.84 g cm<sup>−3</sup>. Continental fragments presently on the ocean floor have an average crustal thickness of 25 km and bulk crustal density of 2.81 g cm<sup>−3</sup>. Accreted allochthonous terranes can be compared to these crustal compilations to better understand which units of crust are accreted or subducted. In general, most accreted terranes are thin crustal units sheared off of FATs and added onto the accretionary prism, with thicknesses on the order of hundreds of meters to a few kilometers. However, many island arcs, oceanic plateaus, and submarine ridges were sheared off in the subduction interface and underplated onto the overlying continent. Other times we find evidence of terrane–continent collision leaving behind accreted terranes 25–40 km thick. We posit that rheologically weak crustal layers or shear zones that were formed when the FATs were produced can be activated as detachments during subduction, allowing parts of the FAT crust to accrete and others to subduct. In many modern FATs on the ocean floor, a sub-crustal layer of high seismic velocities, interpreted as ultramafic material, could serve as a detachment or delaminate during subduction.</p>"/> <meta name="citation_publication_date" content="2014/12/04"/> <meta name="citation_online_date" content="2014/12/04"/> <meta name="citation_journal_title" content="Solid Earth"/> <meta name="citation_volume" content="5"/> <meta name="citation_issue" content="2"/> <meta name="citation_issn" content="1869-9510"/> <meta name="citation_doi" content="https://doi.org/10.5194/se-5-1243-2014"/> <meta name="citation_firstpage" content="1243"/> <meta name="citation_lastpage" content="1275"/> <meta name="citation_author" content="Tetreault, J. L."/> <meta name="citation_author_institution" content="Geodynamics Team, Geological Survey of Norway (NGU), Trondheim, Norway"/> <meta name="citation_author_email" content="joya.tetreault@ngu.no"> <meta name="citation_author" content="Buiter, S. J. 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} #templateSearchResultTerm { font-weight: bold; } #resultsSearchHeader { display: block !important; } #scrolltopmodal { font-size: 3.0em; margin-top: 0 !important; margin-right: 15px; } @-webkit-keyframes animation_dots_breath { 50% { -webkit-transform: scale(1); transform: scale(1); opacity: 1; } 100% { opacity: 0; } } @keyframes animation_dots_breath { 50% { -webkit-transform: scale(1); transform: scale(1); opacity: 1; } 100% { opacity: 0; } } @media (min-width: 768px) and (max-width: 991px) { #templateSearchResultModal .modal-dialog { max-width: 90%; } } </style> <script> if(document.querySelector('meta[name="global_moBaseURL"]').content == "https://meetingorganizer.copernicus.org/") FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder-app')+"search/library.php"; else FINDER_URL = document.querySelector('meta[name="global_moBaseURL"]').content.replace('meetingorganizer', 'finder')+"search/library.php"; SEARCH_INPUT = document.getElementById('search_query_solr'); SEARCH_INPUT_MODAL = document.getElementById('search_query_modal'); searchRunning = false; offset = 20; INITIAL_OFFSET = 20; var MutationObserver = window.MutationObserver || window.WebKitMutationObserver || window.MozMutationObserver; const targetNodeSearchModal = document.getElementById("templateSearchResultModal"); const configSearchModal = { attributes: true, childList: true, subtree: true }; // Callback function to execute when mutations are observed const callbackSearchModal = (mutationList, observer) => { for (const mutation of mutationList) { if (mutation.type === "childList") { // console.log("A child node has been added or removed."); picturesGallery(); } else if (mutation.type === "attributes") { // console.log(`The ${mutation.attributeName} attribute was modified.`); } } }; // Create an observer instance linked to the callback function const observer = new MutationObserver(callbackSearchModal); // Start observing the target node for configured mutations observer.observe(targetNodeSearchModal, configSearchModal); 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L. Tetreault<a href="mailto:joya.tetreault@ngu.no"><i class="fal fa-envelope ml-1"></i></a></span></nobr> <nobr>and <span class="hover-cursor-pointer journal-contentLinkColor hover-underline" data-toggle="modal" data-target=".author280161">S. J. H. Buiter</span></nobr> </div> <div class="modal fade author280160" tabindex="-1" aria-hidden="true"> <div class="modal-dialog modal-dialog-centered modal-dialog-scrollable"> <div class="modal-content"> <div class="modal-header"> <div class="container-fluid p-0"> <h3 class="modal-title">J. L. Tetreault</h3> <div class="row no-gutters"> <div class="col-12">CORRESPONDING AUTHOR</div> <div class="col-12"><a href="mailto:joya.tetreault@ngu.no"><i class="fal fa-envelope mr-2"></i>joya.tetreault@ngu.no</a></div> </div> </div> <button type="button" class="close" data-dismiss="modal" aria-label="Close"> <span aria-hidden="true">×</span> </button> </div> <div class="modal-body"> <div class="container-fluid p-0"> <div class="row"> <div class="col-12 mb-3"> Geodynamics Team, Geological Survey of Norway (NGU), Trondheim, Norway </div> </div> </div> </div> </div> </div> </div> <div class="modal fade author280161" tabindex="-1" aria-hidden="true"> <div class="modal-dialog modal-dialog-centered modal-dialog-scrollable"> <div class="modal-content"> <div class="modal-header"> <div class="container-fluid p-0"> <h3 class="modal-title">S. J. H. Buiter</h3> <div class="row no-gutters"> <div class="col-12"> <a class="orcid-authors-logo" target="_blank" href="https://orcid.org/0000-0002-2493-2377" data-title="https://orcid.org/0000-0002-2493-2377"><svg class="mr-2" version="1.1" xmlns="http://www.w3.org/2000/svg" xmlns:xlink="http://www.w3.org/1999/xlink"><image xlink:href="https://www.solid-earth.net/orcid_icon.svg" src="https://www.solid-earth.net/orcid_icon_128x128.png" width="100%" height="100%"></image></svg>https://orcid.org/0000-0002-2493-2377</a> </div> </div> </div> <button type="button" class="close" data-dismiss="modal" aria-label="Close"> <span aria-hidden="true">×</span> </button> </div> <div class="modal-body"> <div class="container-fluid p-0"> <div class="row"> <div class="col-12 mb-3"> Geodynamics Team, Geological Survey of Norway (NGU), Trondheim, Norway </div> </div> <div class="row"> <div class="col-12 mb-3"> Centre for Earth Evolution and Dynamics, University of Oslo, Oslo, Norway </div> </div> </div> </div> </div> </div> </div> <div class="abstract"> <p><strong class="journal-contentHeaderColor">Abstract.</strong> Allochthonous accreted terranes are exotic geologic units that originated from anomalous crustal regions on a subducting oceanic plate and were transferred to the overriding plate by accretionary processes during subduction. The geographical regions that eventually become accreted allochthonous terranes include island arcs, oceanic plateaus, submarine ridges, seamounts, continental fragments, and microcontinents. These future allochthonous terranes (FATs) contribute to continental crustal growth, subduction dynamics, and crustal recycling in the mantle. We present a review of modern FATs and their accreted counterparts based on available geological, seismic, and gravity studies and discuss their crustal structure, geological origin, and bulk crustal density. Island arcs have an average crustal thickness of 26 km, average bulk crustal density of 2.79 g cm<sup>−3</sup>, and three distinct crustal units overlying a crust–mantle transition zone. Oceanic plateaus and submarine ridges have an average crustal thickness of 21 km and average bulk crustal density of 2.84 g cm<sup>−3</sup>. Continental fragments presently on the ocean floor have an average crustal thickness of 25 km and bulk crustal density of 2.81 g cm<sup>−3</sup>. Accreted allochthonous terranes can be compared to these crustal compilations to better understand which units of crust are accreted or subducted. In general, most accreted terranes are thin crustal units sheared off of FATs and added onto the accretionary prism, with thicknesses on the order of hundreds of meters to a few kilometers. However, many island arcs, oceanic plateaus, and submarine ridges were sheared off in the subduction interface and underplated onto the overlying continent. Other times we find evidence of terrane–continent collision leaving behind accreted terranes 25–40 km thick. We posit that rheologically weak crustal layers or shear zones that were formed when the FATs were produced can be activated as detachments during subduction, allowing parts of the FAT crust to accrete and others to subduct. In many modern FATs on the ocean floor, a sub-crustal layer of high seismic velocities, interpreted as ultramafic material, could serve as a detachment or delaminate during subduction.</p> </div> <div id="oldMobileDownloadBox" class="widget dark-border hide-on-desktop download-and-links"> <div class="legend journal-contentLinkColor">Download & links</div> <div class="content"> <ul class="additional_info no-bullets no-styling"> <li> <a class="triangle" data-toggle=".box-notice" data-duration="300" title="PDF Version (1618 KB)" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.pdf" > Article (PDF, 1618 KB) </a> </li> </ul> </div> </div> <div id="downloadBoxOneColumn" class="widget dark-border hide-on-desktop download-and-links"> <div class="legend journal-contentLinkColor">Download & links</div> <div class="content"> <ul class="additional_info no-bullets no-styling"> <li><a class="triangle" title="PDF Version (1618 KB)" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.pdf">Article</a> <nobr>(1618 KB)</nobr> </li> <li> <a class="triangle" title="XML Version" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.xml">Metadata XML</a> </li> <li><a class="triangle" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.bib">BibTeX</a></li> <li><a class="triangle" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.ris">EndNote</a></li> </ul> </div> </div> <div id="share" class="oneColumnShareMobileBox widget dark-border hide-on-desktop"> <div class="legend journal-contentLinkColor">Share</div> <div class="content row m-0 py-1"> <div class="col-auto pl-0"> <a class="share-one-line" href="https://www.mendeley.com/import/?url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Mendeley" target="_blank"> <img src="https://www.solid-earth.net/mendeley.png" alt="Mendeley"/> </a> </div> <div class="col-auto"> <a class="share-one-line" href="https://www.reddit.com/submit?url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Reddit" target="_blank"> <img src="https://www.solid-earth.net/reddit.png" alt="Reddit"> </a> </div> <div class="col-auto"> <a class="share-one-line last" href="https://twitter.com/intent/tweet?text=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Twitter" target="_blank"> <img src="https://www.solid-earth.net/twitter.png" alt="Twitter"/> </a> </div> <div class="col-auto"> <a class="share-one-line" href="https://www.facebook.com/share.php?u=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F&t=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments" title="Facebook" target="_blank"> <img src="https://www.solid-earth.net/facebook.png" alt="Facebook"/> </a> </div> <div class="col-auto pr-0"> <a class="share-one-line last" href="https://www.linkedin.com/shareArticle?mini=true&url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F&title=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments" title="LinkedIn" target="_blank"> <img src="https://www.solid-earth.net/linkedin.png" alt="LinkedIn"> </a> </div> <div class="col pr-0 mobile-native-share"> <a href="#" data-title="Solid Earth" data-text="*Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments* J. L. Tetreault and S. J. H. Buiter" data-url="https://se.copernicus.org/articles/5/1243/2014/" class="mobile-native-share share-one-line last"><i class="co-mobile-share display-none"></i></a> </div> </div> </div> <div class="citation-footer"> <strong class="journal-contentHeaderColor">How to cite. </strong> Tetreault, J. L. and Buiter, S. J. H.: Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments, Solid Earth, 5, 1243–1275, https://doi.org/10.5194/se-5-1243-2014, 2014. </div> <div id="article-dates" class="sec"> <div class="article-dates dates-content my-3 pb-3"> <nobr>Received: 28 May 2014</nobr> – <nobr>Discussion started: 01 Jul 2014</nobr> – <nobr>Revised: 30 Oct 2014</nobr> – <nobr>Accepted: 04 Nov 2014</nobr> – <nobr>Published: 04 Dec 2014</nobr> </div> </div> </div>  <div class="pswp" tabindex="-1" role="dialog" aria-hidden="true" >  <div class="pswp__bg"></div>  <div class="pswp__scroll-wrap">  <div class="pswp__container"> <div class="pswp__item"></div> <div class="pswp__item"></div> <div class="pswp__item"></div> </div>  <div class="pswp__ui pswp__ui--hidden"> <div class="pswp__top-bar">  <div class="pswp__counter"></div> <button class="pswp__button pswp__button--close" title="Close (Esc)"></button> <button class="pswp__button pswp__button--fs" title="Toggle fullscreen"></button>   <div class="pswp__preloader"> <div class="pswp__preloader__icn"> <div class="pswp__preloader__cut"> <div class="pswp__preloader__donut"></div> </div> </div> </div> </div> <div class="pswp__share-modal pswp__share-modal--hidden pswp__single-tap"> <div class="pswp__share-tooltip"></div> </div> <button class="pswp__button pswp__button--arrow--left" title="Previous (arrow left)"> </button> <button class="pswp__button pswp__button--arrow--right" title="Next (arrow right)"> </button> <div class="pswp__caption "> <div class="pswp__caption__center"></div> </div> </div> </div> </div></div>  <div id="leftColumnExtras" class="CMSCONTAINER w-sidebar col-auto d-none d-lg-block pt-2"> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Download</div> <div class="content"> <ul class="additional_info no-bullets no-styling"> <li><a class="triangle" title="PDF Version (1618 KB)" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.pdf">Article</a> <nobr>(1618 KB)</nobr> </li> <li> <a class="triangle" title="XML Version" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.xml">Metadata XML</a> </li> </ul> </div> <div class="content"> <ul class="additional_info no-bullets no-styling"> <li><a class="triangle" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.bib">BibTeX</a></li> <li><a class="triangle" href="https://se.copernicus.org/articles/5/1243/2014/se-5-1243-2014.ris">EndNote</a></li> </ul> </div> </div> <div class="widget dark-border"> <div class="legend journal-contentLinkColor">Short summary</div> <div class="content hide-js shortSummaryFull">Continents are composed of a collage of accreted terranes: tectonically sutured crustal units of various origins. This review covers the cycle of terrane accretion from the original entity (modern-day oceanic island arcs, oceanic plateaus, submarine ridges, seamounts, continental fragments, and microcontinents) to present-day examples of terrane accretion to finally allochthonous accreted terranes.</div> <div style="display: none" class="content show-js shortSummaryShorten">Continents are composed of a collage of accreted terranes: tectonically sutured crustal units of...</div> <div class="content"> <a href="#" class="more-less show-js triangle" data-hide=".shortSummaryFull" data-show=".shortSummaryShorten" data-toggleCaption='Hide'>Read more</a> </div> </div> <div class="widget dark-border hide-on-mobile hide-on-tablet p-0" id="share"> <div class="legend journal-contentLinkColor">Share</div> <div class="row p-0"> <div class="col-auto pl-0"> <a class="share-one-line" href="https://www.mendeley.com/import/?url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Mendeley" target="_blank"> <img src="https://www.solid-earth.net/mendeley.png" alt="Mendeley"/> </a> </div> <div class="col-auto"> <a class="share-one-line" href="https://www.reddit.com/submit?url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Reddit" target="_blank"> <img src="https://www.solid-earth.net/reddit.png" alt="Reddit"> </a> </div> <div class="col-auto"> <a class="share-one-line last" href="https://twitter.com/intent/tweet?text=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F" title="Twitter" target="_blank"> <img src="https://www.solid-earth.net/twitter.png" alt="Twitter"/> </a> </div> <div class="col-auto"> <a class="share-one-line" href="https://www.facebook.com/share.php?u=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F&t=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments" title="Facebook" target="_blank"> <img src="https://www.solid-earth.net/facebook.png" alt="Facebook"/> </a> </div> <div class="col-auto pr-0"> <a class="share-one-line last" href="https://www.linkedin.com/shareArticle?mini=true&url=https%3A%2F%2Fse.copernicus.org%2Farticles%2F5%2F1243%2F2014%2F&title=Future+accreted+terranes%3A+a+compilation+of+island+arcs%2C+oceanic+plateaus%2C+submarine+ridges%2C+seamounts%2C+and+continental+fragments" title="LinkedIn" target="_blank"> <img src="https://www.solid-earth.net/linkedin.png" alt="LinkedIn"> </a> </div> <div class="col pr-0 mobile-native-share"> <a href="#" data-title="Solid Earth" data-text="*Future accreted terranes: a compilation of island arcs, oceanic plateaus, submarine ridges, seamounts, and continental fragments* J. 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