Geochemical and geophysical constrains on the dynamic topography of the        <fc >S</fc>S        outhern        <fc >A</fc>A        frican        <fc >P</fc>P        lateau

Jones Alan G.; Afonso Juan Carlos; Fullea Javier

摘要

Abstract >The deep mantle African Superswell is considered to contribute to the topographic uplift of the Southern African Plateau, but dynamic support estimates vary wildly depending on the approach and data used. One reason for these large disparities is that the role of lithospheric structure, key in modulating deep dynamic contributions to elevation, is commonly ignored or oversimplified in convection studies. We use multiple high‐quality geophysical data coupled with xenolith‐based geochemical constraints to compute the isostatic lithospheric contribution to the elevation of the Plateau, facilitating isolation of the current dynamic component from the total observed elevation. We employ a multiobservable stochastic algorithm to invert geoid anomaly, surface‐wave dispersion data, magnetotelluric data, and surface heat flow to predict elevation in a fully thermodynamically and internally‐consistent manner. We find that a compositionally layered 230?±?7 km thick lithosphere is required to simultaneously fit all four data types, in agreement with abundant independent xenolith evidence. Our stochastic modeling indicates a lithospheric contribution to elevation of the order of 670 m, which implies dynamic support arising from the convecting sublithospheric mantle of ～650 m. Our results have important implications for the understanding of lithospheric‐deep mantle feedback mechanisms and for calibrating dynamic topography estimates from global convection studies. </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> >深层地幔非洲超级威尔被认为是有助于南部非洲高原的地形隆起，但动态支持估计因使用的方法和数据而异。这些巨大差异的一个原因是岩石结构结构的作用，关键在调节深度动态贡献到升高，通常在对流研究中忽略或过于简化。我们使用多种高质量的地球物理数据与基于Xenolith的地球化学约束相结合，从而计算高原升高的等静压型材贡献，促进了当前动态分量的分离，从总观察到的高度。我们采用多种可操作的随机算法来反转大鼠异常，表面波色散数据，磁识别数据和表面热流，以完全热力学和内部一致的方式预测高度。我们发现一个合成的分层230？±7 km厚的岩石圈需要同时满足所有四种数据类型，同时与丰富的独立Xenolith证据同时符合所有四种数据类型。我们的随机造型表明型号为670米的670米的升高的型贡献，这意味着来自〜650米的对流副间椎间盘的动态支撑。我们的结果对理解岩石树脂深层地幔反馈机制具有重要意义，并用于校准全球对流研究的动态地形估算。</ 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10期</span><b style="margin: 0 2px;">|</b><span>共20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=Jones Alan G.&option=202" target="_blank" rel="nofollow">Jones Alan G.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Afonso Juan Carlos&option=202" target="_blank" rel="nofollow">Afonso Juan Carlos;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fullea Javier&option=202" target="_blank" rel="nofollow">Fullea Javier;</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>Complete MT Solutions Inc.Ottawa Ontario Canada;</p> <p>Department of Earth and Planetary SciencesMacquarie UniversitySydney New South Wales Australia;</p> <p>Dublin Institute for Advanced StudiesDublin Ireland;</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=dynamic topography&option=203" rel="nofollow">dynamic topography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geochemical‐geophysical inversion&option=203" rel="nofollow">geochemical‐geophysical inversion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithosphere&option=203" rel="nofollow">lithosphere;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermochemical modeling&option=203" rel="nofollow">thermochemical modeling;</a> </p> <div class="translation"> 机译：动态地形;地球化学地球物理反演;岩石圈;热化学造型; 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Geochemical and geophysical constrains on the dynamic topography of the SS outhern AA frican PP lateau

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