Crustal Deformation in the India‐Eurasia Collision Zone From 25?Years of GPS Measurements

机译：印度 - 欧亚镇碰撞区的地壳变形从25个？多年的GPS测量

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Abstract >The India‐Eurasia collision zone is the largest deforming region on the planet; direct measurements of present‐day deformation from Global Positioning System (GPS) have the potential to discriminate between competing models of continental tectonics. But the increasing spatial resolution and accuracy of observations have only led to increasingly complex realizations of competing models. Here we present the most complete, accurate, and up‐to‐date velocity field for India‐Eurasia available, comprising 2576 velocities measured during 1991–2015. The core of our velocity field is from the Crustal Movement Observation Network of China‐I/II: 27 continuous stations observed since 1999; 56 campaign stations observed annually during 1998–2007; 1000 campaign stations observed in 1999, 2001, 2004, and 2007; 260 continuous stations operating since late 2010; and 2000 campaign stations observed in 2009, 2011, 2013, and 2015. We process these data and combine the solutions in a consistent reference frame with stations from the Global Strain Rate Model compilation, then invert for continuous velocity and strain rate fields. We update geodetic slip rates for the major faults (some vary along strike), and find that those along the major Tibetan strike‐slip faults are in good agreement with recent geological estimates. The velocity field shows several large undeforming areas, strain focused around some major faults, areas of diffuse strain, and dilation of the high plateau. We suggest that a new generation of dynamic models incorporating strength variations and strain‐weakening mechanisms is required to explain the key observations. Seismic hazard in much of the region is elevated, not just near the major faults. </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> >印度 - 欧亚碰撞区是地球上最大的变形区域;从全球定位系统（GPS）的当前变形的直接测量有可能区分大陆构造的竞争模式。但是，日益增加的空间分辨率和观察的准确性仅导致竞争模型的越来越复杂的实现。在这里，我们为Idia-EuraSia提供了最完整，准确，最新的速度场，包括在1991 - 2015年期间测量的2576个速度。我们的速度场的核心来自中国-I / II的地壳运动观察网络：自1999年以来观察到的27个连续站;在1998 - 2007年期间每年观察到56个竞选站; 1999年，2001年，2004年和2007年观察到的1000个竞选站; 260年度连续车站经营以来，自2010年底以来; 2009年，2011年，2013年和2015年观察到的2000年竞选站。我们处理这些数据并将解决方案与来自全局应变速率模型编译的站点的一致参考帧组合，然后反转连续速度和应变率字段。我们更新大地滑动率为主要断层（沿着罢工有些不同），并发现沿着主要的西藏防滑断层的人与最近的地质估计吻合良好。速度场显示出几个大型的未变形区域，菌株聚焦围绕一些主要断层，漫射菌株的区域，以及高原的扩张。我们建议需要新一代具有强度变化和应变弱化机制的动态模型来解释关键观察。该地区大部分地震危险升高，而不仅仅是在主要断层附近。</ 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23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=Zheng Gang&option=202" target="_blank" rel="nofollow">Zheng Gang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Hua&option=202" target="_blank" rel="nofollow">Wang Hua;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wright Tim J.&option=202" target="_blank" rel="nofollow">Wright Tim J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lou Yidong&option=202" target="_blank" rel="nofollow">Lou Yidong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Rui&option=202" target="_blank" rel="nofollow">Zhang Rui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Weixing&option=202" target="_blank" rel="nofollow">Zhang Weixing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shi Chuang&option=202" target="_blank" rel="nofollow">Shi Chuang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Jinfang&option=202" target="_blank" rel="nofollow">Huang Jinfang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Na&option=202" target="_blank" rel="nofollow">Wei Na;</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>GNSS Research CenterWuhan UniversityWuhan China;</p> <p>Collaborative Innovation Center of Geospatial TechnologyWuhan UniversityWuhan China;</p> <p>COMET School of Earth and EnvironmentUniversity of LeedsLeeds UK;</p> <p>GNSS Research CenterWuhan UniversityWuhan China;</p> <p>National Earthquake Infrastructure ServiceChina Earthquake AdministrationBeijing China;</p> <p>GNSS Research CenterWuhan UniversityWuhan China;</p> <p>GNSS Research CenterWuhan UniversityWuhan China;</p> <p>GNSS Research CenterWuhan UniversityWuhan China;</p> <p>GNSS Research CenterWuhan UniversityWuhan 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=GPS geodesy&option=203" rel="nofollow">GPS geodesy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal deformation&option=203" rel="nofollow">crustal deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=velocity and strain rate fields&option=203" rel="nofollow">velocity and strain rate fields;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fault slip rates&option=203" rel="nofollow">fault slip rates;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=block versus continuum models&option=203" rel="nofollow">block versus continuum models;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=India‐Eurasia collision&option=203" rel="nofollow">India‐Eurasia collision;</a> </p> <div class="translation"> 机译：GPS测地;地壳变形;速度和应变率字段;故障滑移率;块与连续型号;印度 - 欧亚碰撞; </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/0704020651194.html">Crustal Deformation in the India-Eurasia Collision Zone From 25Years of GPS Measurements</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Gang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zheng Gang,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Hua&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Hua,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wright Tim J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wright Tim J.,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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