Delayed Seismicity Rate Changes Controlled by Static Stress Transfer

机译：静态应力转移控制的延迟地震率变化

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Abstract > On 15 June 2010, a M <sub> w </sub> 5.7 earthquake occurred near Ocotillo, California, in the Yuha Desert. This event was the largest aftershock of the 4 April 2010 M <sub> w </sub> 7.2 El Mayor‐Cucapah (EMC) earthquake in this region. The EMC mainshock and subsequent Ocotillo aftershock provide an opportunity to test the Coulomb failure hypothesis (CFS). We explore the spatiotemporal correlation between seismicity rate changes and regions of positive and negative CFS change imparted by the Ocotillo event. Based on simple CFS calculations we divide the Yuha Desert into three subregions, one triggering zone and two stress shadow zones. We find the nominal triggering zone displays immediate triggering, one stress shadowed region experiences immediate quiescence, and the other nominal stress shadow undergoes an immediate rate increase followed by a delayed shutdown. We quantitatively model the spatiotemporal variation of earthquake rates by combining calculations of CFS change with the rate‐state earthquake rate formulation of Dieterich (1994), assuming that each subregion contains a mixture of nucleation sources that experienced a CFS change of differing signs. Our modeling reproduces the observations, including the observed delay in the stress shadow effect in the third region following the Ocotillo aftershock. The delayed shadow effect occurs because of intrinsic differences in the amplitude of the rate response to positive and negative stress changes and the time constants for return to background rates for the two populations. We find that rate‐state models of time‐dependent earthquake rates are in good agreement with the observed rates and thus explain the complex spatiotemporal patterns of seismicity. </p </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 =“JGRB52305-ABS-ABS-0001”XML：LANG =“en”> <标题类型=“main”>抽象</ title> >于2010年6月15日，a <i > m </ i> <sub> w </ i> </ sub> 5.7地震发生在ocotillo，加利福尼亚州，在Yuha沙漠中。该活动是2010年4月4日最大的余震 m </ i> <sub> w </ sub> 7.2 el Mayor-cucapah（EMC）地震。 EMC MainShock和随后的Ocotillo余震提供了测试库仑故障假设（CFS）的机会。我们探讨了Ocotillo事件赋予了ocotillo事件的地震性率变化和积极CFS变化区域之间的时空相关性。基于简单的CFS计算，我们将Yuha沙漠分成三个次区域，一个触发区域和两个应力阴影区域。我们发现标称触发区域立即触发，一个压力阴影区域经历即时静态，另一个标称应力阴影经历立即增加，然后延迟关闭。我们通过将CFS变化的计算与Dieterich（1994）的速率状态变化相结合，定量模拟地震速率的时空变化，假设每个子区域含有经历了不同迹象的CFS变化的成核来源的混合物。我们的建模再现观察结果，包括在Ocotillo余震后第三区中的应力阴影效应中观察到的延迟。由于对正负应力变化的速率响应的幅度和返回到两个人群的背景速率的时间常数，发生延迟的阴影效应。我们发现时间依赖性地震率的速率状态模型与观察到的速率吻合良好，从而解释了地震性的复杂时空模式。 </ 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>2017年第10期</span><b style="margin: 0 2px;">|</b><span>共15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=Kroll Kayla A.&option=202" target="_blank" rel="nofollow">Kroll Kayla A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Richards‐Dinger Keith B.&option=202" target="_blank" rel="nofollow">Richards‐Dinger Keith B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dieterich James H.&option=202" target="_blank" rel="nofollow">Dieterich James H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cochran Elizabeth S.&option=202" target="_blank" rel="nofollow">Cochran Elizabeth S.;</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 CaliforniaRiverside CA USA;</p> <p>Department of Earth SciencesUniversity of CaliforniaRiverside CA USA;</p> <p>Department of Earth SciencesUniversity of CaliforniaRiverside CA USA;</p> <p>Earthquake Science CenterUnited States Geological SurveyPasadena 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=seismicity shutdown&option=203" rel="nofollow">seismicity shutdown;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rate state&option=203" rel="nofollow">rate state;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Coulomb failure&option=203" rel="nofollow">Coulomb failure;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismicity rate increase/decrease&option=203" rel="nofollow">seismicity rate increase/decrease;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=delayed shutdown&option=203" rel="nofollow">delayed shutdown;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=postseismic deformation&option=203" rel="nofollow">postseismic deformation;</a> </p> <div class="translation"> 机译：地震关断;率州;库仑失败;地震率增加/减少;延迟关机;后近的变形; </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/0704020652249.html">Delayed Seismicity Rate Changes Controlled by Static Stress Transfer</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kroll Kayla A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kroll Kayla A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Richards-Dinger Keith B.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Richards-Dinger Keith B.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dieterich James H.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Dieterich James H.,</a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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CARAFA,</a> <span>2011</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：根据大地应变率和统计地震活动确定的静应力下降</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-geophysics_thesis/0201253040324.html">2014年2月12日新疆于田Mw7.0地震源区静态库仑应力变化和地震活动率</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵立波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵立波</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵连锋&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,赵连锋</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=谢小碧&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,谢小碧</a> <span> <a href="/journal-cn-4904/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地球物理学报 </a> </span> <span> . 2016</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_translated-world-seismology_thesis/0201254188227.html">静态应力转移及地震触发：看不到应力下限吗？</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=A.Ziv&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 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Andrew M.Freed1</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=王璞(翻译)2&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,王璞(翻译)2</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=黄禄渊(校对)2&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,黄禄渊(校对)2</a> <span> <a href="/journal-cn-40000/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地壳构造与地壳应力 </a> </span> <span> . 2018</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-673_thesis/020221558689.html">2014年2月12日新疆于田Ms7.3地震源区静态库仑应力变化和地震活动率</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵立波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵立波</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵连锋&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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class="enjiyixqcontent" href="/patent-detail/06120108516077.html">基于横波速度变化率的地应力方位地震预测方法</a> <b>[P]</b> . <span> 中国专利： CN106033127A </span> <span> . 2016-10-19</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130479577458.html">METHOD FOR DETERMINING STATIC TIME DELAYS OF SEISMIC TRACES</a> <b>[P]</b> . <span> 外国专利：  FR2257097B1 </span> <span> . 1979-08-10</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：确定地震迹线静态时间延迟的方法 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130481578767.html">METHOD FOR DETERMINING STATIC TIME DELAYS OF SEISMIC TRACES</a> <b>[P]</b> . <span> 外国专利：  GB1489631A </span> <span> . 1977-10-26</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：确定地震迹线静态时间延迟的方法 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130483727272.html">METHOD FOR DETERMINING STATIC TIME DELAYS OF SEISMIC TRACES</a> <b>[P]</b> . <span> 外国专利：  FR2257097A1 </span> <span> . 1975-08-01</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：确定地震迹线静态时间延迟的方法 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704025592982','4',7,2,1,'',this,24)" class="delivery" prompt="010401" 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