How plume‐ridge interaction shapes the crustal thickness pattern of the        <fc >R</fc>R        éunion hotspot track

Bredow Eva; Steinberger Bernhard; Gassm?ller Rene; Dannberg Juliane

摘要

Abstract >The Réunion mantle plume has shaped a large area of the Earth's surface over the past 65 million years: from the Deccan Traps in India along the hotspot track comprising the island chains of the Laccadives, Maldives, and Chagos Bank on the Indian plate and the Mascarene Plateau on the African plate up to the currently active volcanism at La Réunion Island. This study addresses the question how the Réunion plume, especially in interaction with the Central Indian Ridge, created the complex crustal thickness pattern of the hotspot track. For this purpose, the mantle convection code ASPECT was used to design three‐dimensional numerical models, which consider the specific location of the plume underneath moving plates and surrounded by large‐scale mantle flow. The results show the crustal thickness pattern produced by the plume, which altogether agrees well with topographic maps. Especially two features are consistently reproduced by the models: the distinctive gap in the hotspot track between the Maldives and Chagos is created by the combination of the ridge geometry and plume‐ridge interaction; and the Rodrigues Ridge, a narrow crustal structure which connects the hotspot track and the Central Indian Ridge, appears as the surface expression of a long‐distance sublithospheric flow channel. This study therefore provides further insight how small‐scale surface features are generated by the complex interplay between mantle and lithospheric processes. </abstract> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> <div class="translation abstracttxt"> <span class="zhankaihshouqi fivelineshidden" id="abstract"> <span>机译：</span><Abstract Type =“main”> <标题类型=“main”>抽象</ title> >在过去的6500万年中，réunion披风羽流形成了地球表面的大面积：从印度的德克兰陷阱，包括漆漆，马尔代夫和印度板块的岛屿链条和非洲平板上的睫毛膏高原到了LaRéunion岛目前活跃的火山。这项研究解决了Réunion羽流，特别是与中央印度脊的互动，创造了热点轨道的复杂地壳厚度图案。为此目的，地幔对流代码方面用于设计三维数值模型，其考虑流动板下方的羽流的特定位置，并被大规模的地幔流包围。结果显示了羽流产生的地壳厚度图案，它完全与地形图吻合很好。特别是模型始终再现了两个特征：马尔代夫和焦体之间的热点轨道中的独特差距是由脊几何形状和羽毛脊相互作用的组合而产生的;和罗德里格山脊，连接热点轨道和中央印度脊的狭窄地壳结构看起来作为长距离偏心散流沟道的表面表达。因此，本研究提供了进一步的洞察力，通过地幔和岩石游泳过程之间的复杂相互作用产生了小规模的表面特征。</ p> </摘要> </span> <span class="z_kbtn z_kbtnclass hoverxs" style="display: none;">展开▼</span> </div> </div> <div class="record"> <h2 class="all_title" id="enpatent33" >著录项</h2> <ul> <li> <span class="lefttit">来源</span> <div style="width: 86%;vertical-align: text-top;display: inline-block;"> <a href='/journal-foreign-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2017年第8期</span><b style="margin: 0 2px;">|</b><span>共19页</span> </div> </li> <li> <div class="author"> <span class="lefttit">作者</span> <p id="fAuthorthree" class="threelineshidden zhankaihshouqi"> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bredow Eva&option=202" target="_blank" rel="nofollow">Bredow Eva;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Steinberger Bernhard&option=202" target="_blank" rel="nofollow">Steinberger Bernhard;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gassm?ller Rene&option=202" target="_blank" rel="nofollow">Gassm?ller Rene;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dannberg Juliane&option=202" target="_blank" rel="nofollow">Dannberg Juliane;</a> </p> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zkzz" style="display: none;">展开▼</span> </div> </li> <li> <div style="display: flex;"> <span class="lefttit">作者单位</span> <div style="position: relative;margin-left: 3px;max-width: 639px;"> <div class="threelineshidden zhankaihshouqi" id="fOrgthree"> <p>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>GFZ German Research Centre for GeosciencesPotsdam Germany;</p> <p>Department of MathematicsColorado State UniversityFort Collins Colorado USA;</p> <p>Department of MathematicsColorado State UniversityFort Collins Colorado USA;</p> </div> <span class="z_kbtnclass z_kbtnclassall hoverxs" id="zhdw" style="display: none;">展开▼</span> </div> </div> </li> <li > <span class="lefttit">收录信息</span> <span style="width: 86%;vertical-align: text-top;display: inline-block;"></span> </li> <li> <span class="lefttit">原文格式</span> <span>PDF</span> </li> <li> <span class="lefttit">正文语种</span> <span>eng</span> </li> <li> <span class="lefttit">中图分类</span> <span><a href="https://www.zhangqiaokeyan.com/clc/163.html" title="地球物理学">地球物理学;</a></span> </li> <li class="antistop"> <span class="lefttit">关键词</span> <p style="width: 86%;vertical-align: text-top;"> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=plume‐ridge interaction&option=203" rel="nofollow">plume‐ridge interaction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Réunion mantle plume&option=203" rel="nofollow">Réunion mantle plume;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deccan Traps&option=203" rel="nofollow">Deccan Traps;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hotspot track&option=203" rel="nofollow">hotspot track;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geodynamic model&option=203" rel="nofollow">geodynamic model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indian Ocean&option=203" rel="nofollow">Indian Ocean;</a> </p> <div class="translation"> 机译：Plume-ridge互动;réunion披风羽毛;Deccan Traps;热点轨道;地球节动力模型;印度洋; 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=彭仁&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 彭仁</a> <span> . 2011</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061203526068.html">复杂形状金刚石涂层刀具的HFCVD批量制备方法</a> <b>[P]</b> . <span> 中国专利： CN108559970B </span> <span> . 2019.11.01</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120111059253.html">复杂形状金刚石涂层刀具的HFCVD批量制备方法</a> <b>[P]</b> . <span> 中国专利： CN108559970A </span> <span> . 2018-09-21</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130412272141.html">FC region variants with Properties of Union (neonatal fc receptor (FcRn) and modified Protein to Union held</a> <b>[P]</b> . <span> 外国专利：  AR099080A1 </span> <span> . 2016-06-29</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：具有Union（新生儿fc受体（FcRn）的特性和修饰为Union的蛋白的FC区变体 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130427862597.html">SMALL PEPTIDES CORRESPONDING TO PROTEIN INTERFACE RESIDUES OF PLASMODIUM FALCIPARUM CLPO PROTEASE (PFCLPQ) AND CLPY ATPASE (PFCLPY) OR SMALL DRUG LIKE MOLECULES DESIGNED BASED UPON THESE PEPTIDES THAT INTERFERE WITH INTERFERE WITH INTERACTION OF PFCLPQ AND PFCLPQ AND PFCLPY AS ANTI-MALARIAL DRUGS</a> <b>[P]</b> . <span> 外国专利：  IN2008DE02057A </span> <span> . 2010-04-02</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：对应于恶性疟原虫CLPO蛋白酶（PFCLPQ）和CLPY ATPase（PFCLPY）的蛋白质界面残基的小肽，或基于此类肽设计的小药物分子，它们干扰了PFC和干扰素，干扰了PFC </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130412274431.html">Combining immunoglobulin FC, which maintains the Affinity of Union of the FC Fragment of immunoglobulin to FcRn</a> <b>[P]</b> . <span> 外国专利：  AR096890A1 </span> <span> . 2016-02-03</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：结合免疫球蛋白FC，可维持免疫球蛋白FC片段与FcRn的结合亲和力 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704023360700','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> 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How plume‐ridge interaction shapes the crustal thickness pattern of the RR éunion hotspot track

摘要