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Connecting crustal seismicity and earthquake‐driven stress evolution in Southern California

机译:在南加州连接地壳地震性和地震驱动压力演变

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Abstract > Tectonic stress in the crust evolves during a seismic cycle, with slow stress accumulation over interseismic periods, episodic stress steps at the time of earthquakes, and transient stress readjustment during a postseismic period that may last months to years. Static stress transfer to surrounding faults has been well documented to alter regional seismicity rates over both short and long time scales. While static stress transfer is instantaneous and long lived, postseismic stress transfer driven by viscoelastic relaxation of the ductile lower crust and mantle leads to additional, slowly varying stress perturbations. Both processes may be tested by comparing a decade‐long record of regional seismicity to predicted time‐dependent seismicity rates based on a stress evolution model that includes viscoelastic stress transfer. Here we explore crustal stress evolution arising from the seismic cycle in Southern California from 1981 to 2014 using five M ≥6.5 source quakes: the M 7.3 1992 Landers, M6.5 1992 Big Bear, M 6.7 1994 Big Bear, M 7.1 1999 Hector Mine, and M 7.2 2010 El Mayor‐Cucapah earthquakes. We relate the stress readjustment in the surrounding crust generated by each quake to regional seismicity using rate‐and‐state friction theory. Using a log likelihood approach, we quantify the potential to trigger seismicity of both static and viscoelastic stress transfer, finding that both processes have systematically shaped the spatial pattern of Southern California seismicity since 1992. </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:ID =“JGRB52228-ABS-ABS-ABS-0001”> <标题类型=“main”>摘要</标题> >在地壳期间的地壳中的构造应力在地震循环中发展,慢应力累积过度造型时期,地震时期的情节应力步骤,以及在可能持续数月到几年的后期后期的瞬态应力重新调整。对周围断层的静态应力转移已经充分记录,以改变短期和长时间的区域地震率。虽然静态应力转移是瞬间和长的寿命,但由粘弹性松弛驱动的延性下皮和地幔导致额外,缓慢变化的应力扰动的后颤动的应力转移。可以通过比较基于包括粘弹性应力转移的应力演化模型来比较区域地震性的十个长度记录区域地震性的十个长度记录来进行测试。在这里,我们从1981年到2014年探讨了来自1981年至2014年南部的地震循环引起的地壳压力演进,使用五个 m </ i>≥6.5源quakes: m </ i> 7.3 1992 Landers,M6.5 1992大熊, m </ i> 6.7 1994大熊, m </ i> 7.1 1999 Hectorine,以及 m </ i> 7.2 2010年El Mayor-cucapah地震。我们使用率和状态摩擦理论将每种地区产生的周围地壳中的应力调整联系到区域地震。使用日志似然方法,我们量化了触发静电和粘弹性应力转移的地震性的可能性,发现这两个过程自1992年以来系统地形成了南加州地震性的空间模式。</ 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8期</span><b style="margin: 0 2px;">|</b><span>共18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=Pollitz Fred F.&option=202" target="_blank" rel="nofollow">Pollitz Fred F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cattania Camilla&option=202" target="_blank" rel="nofollow">Cattania Camilla;</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>USGSMenlo Park California USA;</p> <p>GeoForschungsZentrumPotsdam Germany;</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=seismicity&option=203" rel="nofollow">seismicity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crust&option=203" rel="nofollow">crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=viscoelasticity&option=203" rel="nofollow">viscoelasticity;</a> </p> <div class="translation"> 机译:地壳;壳;粘弹性; </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/0704020651924.html">Connecting crustal seismicity and earthquake-driven stress evolution in Southern California</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pollitz Fred F.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pollitz Fred F.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cattania Camilla&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Cattania Camilla </a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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