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首页> 外文期刊>Geochemistry, geophysics, geosystems >Characteristics of the Mantle Flow System Beneath the Indochina Peninsula Revealed by Teleseismic Shear Wave Splitting Analysis
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Characteristics of the Mantle Flow System Beneath the Indochina Peninsula Revealed by Teleseismic Shear Wave Splitting Analysis

机译：由Telesisismic Shear波分裂分析揭示了Indochina半岛下面的地幔流量系统的特征

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Abstract >Numerous geoscientific investigations have been conducted on the southeastern Tibetan Plateau and adjacent areas for understanding crustal and mantle deformation associated with the indentation of the Indian Plate into Eurasia. A number of key issues, such as the causes of a sudden change of fast polarization orientations from N‐S to almost E‐W at approximately 26°N revealed by shear wave splitting (SWS) studies, and the geodynamic implications of the transition still remain enigmatic, partially due to the lack of sufficient SWS measurements on the Indochina Peninsula. Here we employ the SWS technique to systematically illuminate upper mantle anisotropy beneath the Indochina Peninsula with an unprecedented data coverage. The resulting 409 SWS measurements from 29 stations show that upper mantle anisotropy beneath the vast majority of the study area is characterized by dominantly E‐W fast orientations which are nearly orthogonal to the strike of most of the major tectonic features in the study area, ruling out significant lithospheric contributions to the observed anisotropy. This observation, when combined with results from seismic tomography, numerical modeling, surface movement, and focal mechanism investigations, suggests that the observed azimuthal anisotropy is mostly the consequence of absolute plate motion or the westward rollback of the oceanic Indian slab. The flow system induced by the rollback or absolute plate motion may experience regional alteration from mantle upwelling along the eastern edge of the slab and through a previously detected slab window, leading to local variations in the observed splitting parameters. </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> >在西藏高原和邻近地区进行了许多地球科学调查，以了解与印度板材缩进到欧亚大陆的地壳和地幔变形。许多关键问题，例如通过剪切波分裂（SWS）研究显示的大约26°N的N-S突然变化从N-S突然变化的原因。部分地致力于，部分是由于Indochina半岛缺乏足够的SWS测量。在这里，我们采用SWS技术在室外的靛蓝半岛下系统地照亮上部地幔各向异性，具有前所未有的数据覆盖。来自29个站的由此产生的409次SWS测量表明，绝大多数研究区下面的上部地幔各向异性的特点是主要的E-W快速取向，几乎正交到研究区域中的大部分主要构造特征，裁决对观察到的各向异性的重要型岩石贡献。当与地震断层扫描的结果结合起来，数值建模，表面运动和局灶性机制调查结合时，表明观察到的方位角各向异性主要是绝对板运动的后果或海洋印度板的向西回滚。由回滚或绝对板运动引起的流动系统可能会沿着板坯的东边缘和通过先前检测到的平板窗口的地幔升高的区域改变，导致观察到的分裂参数中的局部变化。</ 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5期</span><b style="margin: 0 2px;">|</b><span>共14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=Yu Youqiang&option=202" target="_blank" rel="nofollow">Yu Youqiang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Stephen S.&option=202" target="_blank" rel="nofollow">Gao Stephen S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Kelly H.&option=202" target="_blank" rel="nofollow">Liu Kelly H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Ting&option=202" target="_blank" rel="nofollow">Yang Ting;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xue Mei&option=202" target="_blank" rel="nofollow">Xue Mei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Le Khanh Phon&option=202" target="_blank" rel="nofollow">Le Khanh Phon;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Jinyao&option=202" target="_blank" rel="nofollow">Gao Jinyao;</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>State Key Laboratory of Marine GeologyTongji UniversityShanghai China;</p> <p>Geology and Geophysics ProgramMissouri University of Science and TechnologyRolla Missouri USA;</p> <p>Geology and Geophysics ProgramMissouri University of Science and TechnologyRolla Missouri USA;</p> <p>School of OceanographySouthern University of Science and TechnologyShenzhen China;</p> <p>State Key Laboratory of Marine GeologyTongji UniversityShanghai China;</p> <p>Faculty of Oil and GasHanoi University of Mining and GeologyHanoi Vietnam;</p> <p>Second Institute of Oceanography State Oceanic AdministrationHangzhou China;</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=Indochina Peninsula&option=203" rel="nofollow">Indochina Peninsula;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction&option=203" rel="nofollow">subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=shear wave splitting&option=203" rel="nofollow">shear wave splitting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=slab rollback&option=203" rel="nofollow">slab rollback;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=APM&option=203" rel="nofollow">APM;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle flow&option=203" rel="nofollow">mantle flow;</a> </p> <div class="translation"> 机译：吲哚china半岛;俯冲;剪切波分裂;板簧回滚;APM;披风流动; </div> </li> </ul> </div> </div> <div class="literature cardcommon"> <div class="similarity "> <h3 class="all_title" id="enpatent66">相似文献</h3> <div class="similaritytab clearfix"> <ul> <li class="active" >外文文献</li> <li >中文文献</li> <li >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360530.html">Characteristics of the Mantle Flow System Beneath the Indochina Peninsula Revealed by Teleseismic Shear Wave Splitting Analysis</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yu Youqiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yu Youqiang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Stephen S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gao Stephen S.,</a> <a 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