Imaging Lithospheric Discontinuities Beneath the Northern East African Rift Using        <i >SS        ‐to‐        <i >PP        Receiver Functions

Lavayssière Aude; Rychert Catherine; Harmon Nicholas; Keir Derek; Hammond James O. S.; Kendall J.‐Michael; Doubre Cécile; Leroy Sylvie

摘要

Abstract > Imaging the lithosphere is key to understand mechanisms of extension as rifting progresses. Continental rifting results in a combination of mechanical stretching and thinning of the lithosphere, decompression upwelling, heating, sometimes partial melting of the asthenosphere, and potentially partial melting of the mantle lithosphere. The northern East African Rift system is an ideal locale to study these processes as it exposes the transition from tectonically active continental rifting to incipient seafloor spreading. Here we use S ‐to‐ P receiver functions to image the lithospheric structure beneath the northernmost East African Rift system where it forms a triple junction between the Main Ethiopian rift, the Red Sea rift, and the Gulf of Aden rift. We image the Moho at 31?±?6?km beneath the Ethiopian plateau. The crust is 28?±?3?km thick beneath the Main Ethiopian rift and thins to 23?±?2?km in northern Afar. We identify a negative phase, a velocity decrease with depth, at 67?±?3 km depth beneath the Ethiopian plateau, likely associated with the lithosphere‐asthenosphere boundary (LAB), and a lack of a LAB phase beneath the rift. Using observations and waveform modeling, we show that the LAB phase beneath the plateau is likely defined by a small amount of partial melt. The lack of a LAB phase beneath the rift suggests melt percolation through the base of the lithosphere beneath the northernmost East African Rift system. </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”XML：Lang =“en”> <标题类型=“main”>抽象</ title> > 成像岩石圈是理解延伸机制作为渔罗的进展的关键。大陆渔矿导致机械拉伸和岩石圈，减压升高，加热，加热，有时部分熔化的近距离岩石的组合，以及岩石圈的潜在部分熔化。北方的非洲裂谷系统是一个理想的地区，以研究这些过程，因为它暴露了从根本活跃的大陆河流到初期海底蔓延的过渡。我们在这里使用 s </ i> -到- p </ i> 接收器用来将北部的东非裂谷系统下方的岩石空间结构形象在其中，它在主要的埃塞俄比亚裂谷，红海裂谷和亚丁裂谷的湾之间形成了三倍。我们在埃塞俄比亚高原下面的31次图像±6？Km。地壳是28°？我们识别出负阶段，速度随深度减少，在埃塞俄比亚高原下面的67±3公里深度，可能与岩石圈的近距离界面（实验室）有关，并且缺乏裂谷下面的实验室阶段。使用观测和波形建模，我们表明平台下方的实验室相位可能由少量的部分熔体定义。裂谷下面的实验室阶段缺乏通过北部最北部非洲裂口系统下岩石圈的基础融化。 </ 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>2018年第10期</span><b style="margin: 0 2px;">|</b><span>共15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=Lavayssière Aude&option=202" target="_blank" rel="nofollow">Lavayssière Aude;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rychert Catherine&option=202" target="_blank" rel="nofollow">Rychert Catherine;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harmon Nicholas&option=202" target="_blank" rel="nofollow">Harmon Nicholas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Keir Derek&option=202" target="_blank" rel="nofollow">Keir Derek;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hammond James O. S.&option=202" target="_blank" rel="nofollow">Hammond James O. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kendall J.‐Michael&option=202" target="_blank" rel="nofollow">Kendall J.‐Michael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Doubre Cécile&option=202" target="_blank" rel="nofollow">Doubre Cécile;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leroy Sylvie&option=202" target="_blank" rel="nofollow">Leroy Sylvie;</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>National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>Department of Earth and Planetary Sciences BirkbeckUniversity of LondonLondon UK;</p> <p>School of Earth SciencesUniversity of BristolBristol UK;</p> <p>Institut de Physique du Globe de Strasbourg UMR 7516Université de Strasbourg/EOST CNRSStrasbourg France;</p> <p>CNRS UMR 7193 Institut des Sciences de la Terre de ParisSorbonne UniversitéParis France;</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=East African rift&option=203" rel="nofollow">East African rift;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithosphere‐asthenosphere boundary&option=203" rel="nofollow">lithosphere‐asthenosphere boundary;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=continental rifting&option=203" rel="nofollow">continental rifting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=receiver functions&option=203" rel="nofollow">receiver functions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=partial melt&option=203" rel="nofollow">partial melt;</a> </p> <div class="translation"> 机译：东非裂谷;岩石圈 - 哮喘圈边界;大陆河流;接收器功能;部分熔体; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> 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Imaging Lithospheric Discontinuities Beneath the Northern East African Rift Using SS ‐to‐ PP Receiver Functions

摘要