Neotectonic Deformation in Central Eurasia: A Geodynamic Model Approach

机译：欧亚中部的新插孔变形：地球动力学模型方法

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Abstract >Central Eurasia hosts wide orogenic belts of collision between India and Arabia with Eurasia, with diffuse or localized deformation occurring up to hundreds of kilometers from the primary plate boundaries. Although numerous studies have investigated the neotectonic deformation in central Eurasia, most of them have focused on limited segments of the orogenic systems. Here we explore the neotectonic deformation of all of central Eurasia, including both collision zones and the links between them. We use a thin‐spherical sheet approach in which lithosphere strength is calculated from lithosphere structure and its thermal regime. We investigate the contributions of variations in lithospheric structure, rheology, boundary conditions, and fault friction coefficients on the predicted velocity and stress fields. Results (deformation pattern, surface velocities, tectonic stresses, and slip rates on faults) are constrained by independent observations of tectonic regime, GPS, and stress data. Our model predictions reproduce the counterclockwise rotation of Arabia and Iran, the westward escape of Anatolia, and the eastward extrusion of the northern Tibetan Plateau. To simulate the observed extensional faults in the Tibetan Plateau, a weaker lithosphere is required, provided by a change in the rheological parameters. The southward movement of the SE Tibetan Plateau can be explained by the combined effects of the Sumatra trench retreat, a thinner lithospheric mantle, and strik‐slip faults in the region. This study offers a comprehensive model for regions with little or no data coverage, like the Arabia‐India intercollision zone, where the surface velocity is northward showing no deflection related to Arabia and India indentations. </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”> <Title Type =“Main”> Abstract </ Title> <P>中央欧亚西亚举办了印度和阿拉伯与欧亚大陆，欧亚大陆之间的宽organic带宽阔的敌人变形距离初级板边界高达数百公里。虽然许多研究已经调查了欧亚亚洲中部的新推位变形，但大多数都集中在敌人系统的有限细胞上。在这里，我们探讨了欧亚中部所有中部的新发现变形，包括碰撞区和它们之间的联系。我们使用薄型球形薄片方法，其中岩石圈强度由岩石圈结构及其热调节计算。我们研究了岩石结构结构，流变学，边界条件和故障摩擦系数对预测速度和应力场的贡献。结果（变形图案，表面速度，构造应力和故障的滑移率）受到对构造制度，GPS和应力数据的独立观察来约束。我们的模型预测再现了阿拉伯和伊朗的逆时针，安纳托利亚向西逃离，北北北北方高原的东部挤出。为了模拟藏高平台的观察到的延伸断层，需要较弱的岩石圈，通过流变参数的变化提供。 SEIBETAN高原的南方运动可以通过苏门答腊沟槽撤退，较薄的岩石型罩和该地区的Strik-Slip断层的综合影响来解释。本研究为数据覆盖率很少或没有数据覆盖的地区提供了全面的型号，如阿拉伯 - 印度间Intercollision区，这里的表面速度向北显示没有与阿拉伯和印度缩进相关的偏转。</ 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>2017年第11期</span><b style="margin: 0 2px;">|</b><span>共24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=Tunini Lavinia&option=202" target="_blank" rel="nofollow">Tunini Lavinia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiménez‐Munt Ivone&option=202" target="_blank" rel="nofollow">Jiménez‐Munt Ivone;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fernandez Manel&option=202" target="_blank" rel="nofollow">Fernandez Manel;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vergés Jaume&option=202" target="_blank" rel="nofollow">Vergés Jaume;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bird Peter&option=202" target="_blank" rel="nofollow">Bird Peter;</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>Group of Dynamics of the LithosphereInstitute of Earth Sciences Jaume Almera CSICBarcelona Spain;</p> <p>Group of Dynamics of the LithosphereInstitute of Earth Sciences Jaume Almera CSICBarcelona Spain;</p> <p>Group of Dynamics of the LithosphereInstitute of Earth Sciences Jaume Almera CSICBarcelona Spain;</p> <p>Group of Dynamics of the LithosphereInstitute of Earth Sciences Jaume Almera CSICBarcelona Spain;</p> <p>Department of Earth Planetary and Space SciencesUniversity of CaliforniaLos Angeles CA USA;</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=Himalaya&option=203" rel="nofollow">Himalaya;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zagros&option=203" rel="nofollow">Zagros;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tibet&option=203" rel="nofollow">Tibet;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=geodynamic&option=203" rel="nofollow">geodynamic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=deformation&option=203" rel="nofollow">deformation;</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> </p> <div class="translation"> 机译：喜马拉雅;Zagros;西藏;地球动力学;变形;岩石圈; </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/0704020651835.html">Neotectonic Deformation in Central Eurasia: A Geodynamic Model Approach</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tunini Lavinia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tunini Lavinia,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jimenez-Munt Ivone&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Jimenez-Munt Ivone,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fernandez Manel&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Fernandez Manel,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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