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Impulsive Source of the 2017 MM W WW =7.3 Ezgeleh, Iran, Earthquake

机译:2017年的脉冲来源 m m w w = 7.3 ezgeleh,伊朗,地震

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Abstract > On 12 November 2017, a <fi>M</fi> <sub> <fi>W</fi> </sub> =7.3 earthquake struck near the Iranian town of Ezgeleh, at the Iran‐Iraq border. This event was located within the Zagros fold and thrust belt which delimits the continental collision between the Arabian and Eurasian Plates. Despite a high seismic risk, the seismogenic behavior of the complex network of active faults is not well documented in this area due to the long recurrence interval of large earthquakes. In this study, we jointly invert interferometric synthetic aperture radar and near‐field strong motions to infer a kinematic slip model of the rupture. The incorporation of these near‐field observations enables a fine resolution of the kinematic rupture process. It reveals an impulsive seismic source with a strong southward rupture directivity, consistent with significant damage south of the epicenter. We also show that the slip direction does not match plate convergence, implying that some of the accumulated strain must be partitioned onto other 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”xml:id =“grl58975-abs-abs-0001”> <标题类型=“main”> abstract </ title> >于2017年11月12日,a <fi > m </ fi> <sub> <fi> w </ fi> </ sub> = 7.3地震袭击了伊朗伊拉克边境伊朗镇伊朗镇伊朗镇的地震。该事件位于Zagros折叠和推力带内,占据阿拉伯和欧亚板块之间的大陆碰撞。尽管存在高地震风险,但由于大地震的长期复发间隔,在该地区的复杂活性断层网络的发震行为并不充分记录。在这项研究中,我们共同反转干涉机合成孔径雷达和近场强运动,以推断出破裂的运动滑动模型。结合这些近场观察能够精细分辨运动破裂过程。它揭示了一种强烈的南方破裂方向性的冲动的地震源,符合震中南部的重大损害。我们还表明,滑动方向不匹配板收敛,这意味着一些累积的应变必须将其划分为其他故障。 </ p> </ abstract> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第10期</span><b style="margin: 0 2px;">|</b><span>共10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=Gombert B.&option=202" target="_blank" rel="nofollow">Gombert B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Duputel Z.&option=202" target="_blank" rel="nofollow">Duputel Z.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shabani E.&option=202" target="_blank" rel="nofollow">Shabani E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rivera L.&option=202" target="_blank" rel="nofollow">Rivera L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jolivet R.&option=202" target="_blank" rel="nofollow">Jolivet R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hollingsworth J.&option=202" target="_blank" rel="nofollow">Hollingsworth J.;</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>Department of Earth SciencesUniversity of OxfordOxford UK;</p> <p>Institut de Physique du Globe de Strasbourg UMR7516Université de Strasbourg EOST/CNRSStrasbourg France;</p> <p>Department of Seismology Institute of GeophysicsUniversity of TehranTehran Iran;</p> <p>Institut de Physique du Globe de Strasbourg UMR7516Université de Strasbourg EOST/CNRSStrasbourg France;</p> <p>Laboratoire de géologie Département de Géosciences école Normale SupérieurePSL Research University CNRS UMR 8538Paris France;</p> <p>ISTerre/CNRS UMR5275Université Grenoble AlpesGrenoble France;</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=earthquake source physics&option=203" rel="nofollow">earthquake source physics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tectonics&option=203" rel="nofollow">tectonics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zagros Thrust and Fold Belt&option=203" rel="nofollow">Zagros Thrust and Fold Belt;</a> </p> <div class="translation"> 机译:地震源物理;构造;ZAGROS推力和折叠带; 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