Seismic Imaging of Lithosphere Structure and Upper Mantle Deformation Beneath East‐Central China and Their Tectonic Implications

Li Hongyi; Song Xiaodong; Lü Qingtian; Yang Xiaoyu; Deng Yangfan; Ouyang Longbin; Li Jiapeng; Li Xinfu; Jiang Guoming

摘要

Abstract >We conduct a nonlinear joint inversion of receiver functions and surface waves to obtain the lithosphere structure in east‐central China. We also use SKS splitting measurements to evaluate upper mantle deformation. The velocity model reveals that, to the east of the North‐South Gravity Lineament, the crust and lithosphere are significantly thinned. Three extensive crustal/lithospheric thinning subregions are identified. This indicates that the lithospheric modification in east‐central China is nonuniform due to heterogeneity of lithospheric strength. Extensive crustal and lithospheric thinning probably occurs in some weak zones such as basin‐range junction belts and large faults. The structure beneath the Dabie orogenic belt is complex due to the collision between the North and South China Blocks during the Late Paleozoic‐Triassic. The Dabie orogenic belt is delineated by a thick crust with a midcrust low‐velocity zone and a two‐directional convergence in the lithospheric scale. The crust and uppermost mantle across the Tanlu fault exhibit a strong seismic velocity contrast, which suggests deep penetration of this lithospheric‐scale fault. Most of our splitting measurements show nearly E‐W trending fast polarization. The similar present‐day lithosphere structure and upper mantle deformation may imply that the eastern North China Craton and South China Block have been dominated by a common dynamic process since the Late Mesozoic. The westward subduction of the Philippine plate and the long‐range effects of the collision between the Indian and Eurasia plates during the Cenozoic may have also contributed to the present velocity structure and stress field of eastern China. </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> >我们进行接收器功能和表面波的非线性关节反转，以获得东部的岩石圈结构 - 中央中国。我们还使用SKS分裂测量来评估上部地幔变形。速度模型揭示了，向东北重力线的东部，地壳和岩石圈显着变薄。鉴定了三个广泛的地壳/岩石树脂稀疏子区域。这表明由于岩石术强度的异质性，中国东部的岩石术改性是不均匀的。广泛的地壳和岩石树脂稀疏可能发生在一些弱区内，如盆地连接带和大故障。由于北部古生代 - 三叠纪的南部和华南区块之间的碰撞，Dabie Orogenic皮带下方的结构很复杂。 Dabie Orogenicab皮带通过厚的地壳划清，具有半圆形低速区和岩石尺度的双向收敛。 Tanlu故障的地壳和最上面的地幔表现出强烈的地震速度对比度，这表明这种岩石尺度故障深入渗透。我们的大部分分裂测量显示了几乎E-W趋势快速极化。类似的现在岩石圈结构和上部地幔变形可能意味着自中生代晚期以来，东北克拉顿和华南地区一直由共同的动态过程主导。菲律宾板的向西介绍和新生代印度和欧亚邦的碰撞之间的碰撞的远程影响也可能导致中国东部的目前的速度结构和应力场。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第4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=Li Hongyi&option=202" target="_blank" rel="nofollow">Li Hongyi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Song Xiaodong&option=202" target="_blank" rel="nofollow">Song Xiaodong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lü Qingtian&option=202" target="_blank" rel="nofollow">Lü Qingtian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Xiaoyu&option=202" target="_blank" rel="nofollow">Yang Xiaoyu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Yangfan&option=202" target="_blank" rel="nofollow">Deng Yangfan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ouyang Longbin&option=202" target="_blank" rel="nofollow">Ouyang Longbin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Jiapeng&option=202" target="_blank" rel="nofollow">Li Jiapeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Xinfu&option=202" target="_blank" rel="nofollow">Li Xinfu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiang Guoming&option=202" target="_blank" rel="nofollow">Jiang Guoming;</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 Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing China;</p> <p>Department of GeologyUniversity of Illinois at Urbana‐ChampaignUrbana IL USA;</p> <p>SinoProbe Center‐China Deep Exploration CenterChinese Academy of Geological SciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral Resources School of Geophysics and Information TechnologyChina University of GeosciencesBeijing 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=joint inversion&option=203" rel="nofollow">joint inversion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=SKS wave splitting&option=203" rel="nofollow">SKS wave splitting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crust and uppermost mantle structure&option=203" rel="nofollow">crust and uppermost mantle structure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=east‐Central China&option=203" rel="nofollow">east‐Central China;</a> </p> <div class="translation"> 机译：联合反演;SKS波分裂;地壳和最高的地幔结构;中国东部; 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Yibo Wang1</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jialiang Xu1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Jialiang Xu1</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Songlei Xie1&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Songlei Xie1</a> <span> <a href="/journal-cn-39438/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 海洋地质 </a> </span> <span> . 2017</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geology-in-china_thesis/0201252104382.html">瑞雷-泰勒不稳定性与中国东部岩石圈——三论岩石圈地幔蘑菇云构造</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=袁学诚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 袁学诚</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李善芳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李善芳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=管烨&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,管烨</a> <span> <a href="/journal-cn-4800/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地质 </a> </span> <span> . 2012</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-3927_thesis/02022909686.html">青藏高原东北缘与外围克拉通构造转换区的岩石圈结构与构造变形</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高锐&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 高锐</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王海燕&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王海燕</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭晓玉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郭晓玉</a> <span> <a href="/conference-cn-3927/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2014年中国地球科学联合学术年会 </a> <span> <span> . 2014</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020314352124.html">地壳及上地幔深部结构地震成像研究——以阿拉斯加俯冲带和龙门山构造带为例</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=柳存喜&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 柳存喜</a> <span> . 2015</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06120113989185.html">基于差异构造变形模拟的地震成像方法及装置</a> <b>[P]</b> . <span> 中国专利： CN114076984A </span> <span> . 2022-02-22</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120209779181.html">抵抗大变形的地下结构变形缝防水构造</a> <b>[P]</b> . <span> 中国专利： CN209779706U </span> <span> . 2019.12.13</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130416591224.html">Tectonic model of seismic zones in the continental lithosphere of the earth. METHOD OF CONSTRUCTION AND USE OF MODELS tectonic seismic zones in the continental lithosphere EARTH</a> <b>[P]</b> . <span> 外国专利：  RU2013116281A </span> <span> . 2014-10-20</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：地球大陆岩石圈地震带的构造模型。大陆岩石圈地球构造地震带模型的构建和使用方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130425466953.html">In the absorber project, there is a central longitudinal line, an orthogonal central transverse line and the upper line. The upper side is opposite to the next side, and contains the upper layer and at least three color areas in geometric shape. They gathered in a focus area.</a> <b>[P]</b> . <span> 外国专利：  CL2009001106A1 </span> <span> . 2010-12-24</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：在吸收器项目中，有一条中心纵线，一条正交的中心横线和一条上线。上侧与下侧相对，并包含上层和至少三个几何形状的颜色区域。他们聚集在一个重点领域。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130439046991.html">Deformation element for motor vehicle has spatial structure with at least one structured absorption region for introducing deformations that runs around body of deformation element in form of spiral</a> <b>[P]</b> . <span> 外国专利：  DE202004009916U1 </span> <span> . 2005-08-11</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：机动车的变形元件具有空间结构，该空间结构具有至少一个结构化的吸收区域，用于引入以螺旋形式围绕变形元件的主体延伸的变形 </span> </p> </li> 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