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Spatial and Temporal Evolution of Earthquake Dynamics: Case Study of the MM w ww 8.3 Illapel Earthquake, Chile

机译：地震动力学的空间和时间演进：案例研究 m w w 8.3 illapel地震，智利

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Abstract > We develop a methodology that combines compressive sensing backprojection (CS‐BP) and source spectral analysis of teleseismic <fi>P</fi> waves to provide metrics relevant to earthquake dynamics of large events. We improve the CS‐BP method by an autoadaptive source grid refinement as well as a reference source adjustment technique to gain better spatial and temporal resolution of the locations of the radiated bursts. We also use a two‐step source spectral analysis based on (i) simple theoretical Green's functions that include depth phases and water reverberations and on (ii) empirical <fi>P</fi> wave Green's functions. Furthermore, we propose a source spectrogram methodology that provides the temporal evolution of dynamic parameters such as radiated energy and falloff rates. Bridging backprojection and spectrogram analysis provides a spatial and temporal evolution of these dynamic source parameters. We apply our technique to the recent 2015 <fi>M</fi> <sub> <fi>w</fi> </sub> 8.3 megathrust Illapel earthquake (Chile). The results from both techniques are consistent and reveal a depth‐varying seismic radiation that is also found in other megathrust earthquakes. The low‐frequency content of the seismic radiation is located in the shallow part of the megathrust, propagating unilaterally from the hypocenter toward the trench while most of the high‐frequency content comes from the downdip part of the fault. Interpretation of multiple rupture stages in the radiation is also supported by the temporal variations of radiated energy and falloff rates. Finally, we discuss the possible mechanisms, either from prestress, fault geometry, and/or frictional properties to explain our observables. Our methodology is an attempt to bridge kinematic observations with earthquake dynamics. </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> >我们开发一种结合压缩感测反向分子（CS-BP）和源谱分析的方法Telesmicic <Fi> P </ Fi>波浪提供与大型事件的地震动态相关的指标。我们通过Autoadaptive源电网细化以及参考源调整技术来改进CS-BP方法，以获得辐射突发位置的更好的空间和时间分辨率。我们还使用基于（i）简单的理论绿色功能的两步源谱分析，包括深度阶段和水混响以及（ii）经验<fi> p </ fi>波浪绿色的功能。此外，我们提出了一种源谱图方法，该方法提供动态参数的时间演变，例如辐射能量和衰减率。桥接背部分析和频谱图分析提供了这些动态源参数的空间和时间演变。我们将技术应用于最近的2015年<fi> m </ fi> <sub> <fi> w </ sub> 8.3 megathrust illapel地震（智利）。两种技术的结果是一致的，并揭示了在其他巨大地震中发现的深度变化的地震辐射。地震辐射的低频含量位于Megothrust的浅部分中，在大多数高频内容中从低静脉传播到沟槽的距离，而大多数高频含量来自故障的下层部分。辐射能量和衰减速率的时间变化也支持辐射中多次破裂阶段的解释。最后，我们讨论了来自预应力，故障几何和/或摩擦性质的可能机制来解释我们的观察到。我们的方法是试图通过地震动态来建立运动学观测。 </ p> </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1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=Yin Jiuxun&option=202" target="_blank" rel="nofollow">Yin Jiuxun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Denolle Marine A.&option=202" target="_blank" rel="nofollow">Denolle Marine A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Huajian&option=202" target="_blank" rel="nofollow">Yao Huajian;</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 and Planetary SciencesHarvard UniversityCambridge MA USA;</p> <p>Department of Earth and Planetary SciencesHarvard UniversityCambridge MA USA;</p> <p>Laboratory of Seismology and Physics of Earth's Interior and School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei 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=Illapel Earthquake&option=203" rel="nofollow">Illapel Earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=radiated energy&option=203" rel="nofollow">radiated energy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=backprojection&option=203" rel="nofollow">backprojection;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake dynamics&option=203" rel="nofollow">earthquake dynamics;</a> </p> <div class="translation"> 机译：伊芙兰地震;辐射能量;背投;地震动力学; </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/0704025592887.html">Spatial and Temporal Evolution of Earthquake Dynamics: Case Study of the <i >MM <sub > w </sub> <i >ww 8.3 Illapel Earthquake, Chile</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yin Jiuxun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yin Jiuxun,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Denolle Marine A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Denolle Marine A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Huajian&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yao Huajian </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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