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首页> 外文期刊>Geochemistry, geophysics, geosystems >Seismic Evidence for Lateral Asthenospheric Flow Beneath the Northeastern Tibetan Plateau Derived From SS Receiver Functions
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Seismic Evidence for Lateral Asthenospheric Flow Beneath the Northeastern Tibetan Plateau Derived From SS Receiver Functions

机译：东北藏高原下方侧面哮喘流动的地震证据来自 s s 接收器功能

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摘要

Abstract > We present detailed lithospheric images of the NE Tibetan Plateau by applying the depth migration technique to S receiver functions derived from 113 broadband stations. Our migrated images indicate that the lithosphere‐asthenosphere boundary (LAB) lies at depths of 105–120?km beneath the Qilian terrane and reaches depths of 126–140?km below the Alxa and Ordos blocks. The most prominent variation in the LAB depth is the presence of LAB steps of no less than 20?km in the transition zone between the active NE Tibetan Plateau and the surrounding cratonic Alxa and Ordos blocks, which conflicts with the model of southward subduction of the Alxa and Ordos blocks. Furthermore, the marked LAB steps occur at 130?±?10?km away from the southern surficial boundary faults between the NE Tibetan Plateau and the surrounding tectonic provinces, corresponding to the North Qilian fault and the Liupanshan fault, respectively. Therefore, we propose that these scenarios of LAB can be attributed to the delamination of fragmented mantle lithosphere in the transition zone between the NE Tibetan Plateau and the surrounding Alxa and Ordos blocks, triggered by lateral asthenospheric flow. In addition, our observations of a thin lithosphere with thickness of 107–115?km beneath the Songpan‐Ganzi terrane and the west Qinlin orogen greatly facilitate the process of underlying lateral asthenospheric flow. The isostatic uplift of the plateau caused by the delamination of fragmented mantle lithosphere, together with increased horizontal compressive stress, may have led to the outward growth of the NE Tibetan Plateau. </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> > 我们通过应用深度迁移技术呈现NEIBETAN高原的详细岩石图像 s </ i> 从113个宽带站导出的接收器函数。我们迁移的图像表明岩石圈 - 哮喘圈边界（实验室）在祁连地区下面的深度为105-120？Km，达到了Alxa和Ordos块下方126-140 km的深度。实验室深度中最突出的变化是有源网藏高原平台和周围的克拉索阿克萨和鄂尔多斯街区之间的过渡区内的实验室步骤的存在不低于20 km，这与南部俯冲模型冲突Alxa和Ordos块。此外，标记的实验室步骤发生在130？±10.千里，远离南部曲线平台和周围构造省份之间的南方曲线界面，分别对应于北祁连故障和六山山故障。因此，我们提出这些实验室的这种情况可归因于NEIBETAN平台和周围的ALXA和ORDOS块之间的过渡区中分散的地幔岩石层的分层，由横向哮喘流动引发。此外，我们在松潘 - 甘孜地区厚度为107-115的薄层圈和西秦林orenogen的观察，厚度为107-115厘米，极大地促进了潜在的横向哮喘流动的过程。由分散的裂缝岩石圈的分层引起的高原的等静压隆起，以及增加水平压缩应力，可能导致了NEIBETAN高原的向外生长。 </ 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>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共12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=Xu Qiang&option=202" target="_blank" rel="nofollow">Xu Qiang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pei Shunping&option=202" target="_blank" rel="nofollow">Pei Shunping;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuan Xiaohui&option=202" target="_blank" rel="nofollow">Yuan Xiaohui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Junmeng&option=202" target="_blank" rel="nofollow">Zhao Junmeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Hongbing&option=202" target="_blank" rel="nofollow">Liu Hongbing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tu Hongwei&option=202" target="_blank" rel="nofollow">Tu Hongwei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Shuze&option=202" target="_blank" rel="nofollow">Chen Shuze;</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>Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>Deutsches GeoForschungsZentrum GFZ TelegrafenbergPotsdam Germany;</p> <p>Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing China;</p> <p>Earthquake Administration of QianghaiXining China;</p> <p>Key Laboratory of Continental Collision and Plateau Uplift Institute of Tibetan Plateau ResearchChinese Academy of SciencesBeijing 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=S receiver functions&option=203" rel="nofollow">S receiver functions;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=depth migration technique&option=203" rel="nofollow">depth migration technique;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LAB&option=203" rel="nofollow">LAB;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=northeastern Tibetan Plateau&option=203" rel="nofollow">northeastern Tibetan Plateau;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=asthenospheric flow&option=203" rel="nofollow">asthenospheric flow;</a> </p> <div class="translation"> 机译：S接收器功能;深度迁移技术;实验室;藏族高原东北部;哮喘流动; </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/0704023360517.html">Seismic Evidence for Lateral Asthenospheric Flow Beneath the Northeastern Tibetan Plateau Derived From <i >SS Receiver Functions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Qiang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xu Qiang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pei Shunping&option=202" 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