Earthquake Stress Drop and Arias Intensity

机译：地震应力下降和咏叹调强度

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Abstract > We determine earthquake stress drops directly from the Arias intensity database of NGA‐West2. Arias intensity (Arias, 1970, <url href="https://www.osti.gov/biblio/4167721">https://www.osti.gov/biblio/4167721</url> ) is an engineering measure proportional to the integral of the absolute value of acceleration squared, over the significant duration of the signal. As such, it is closely related to root mean square acceleration and can readily be connected to earthquake stress drop (Hanks & McGuire, 1981, <url href="https://pubs.geoscienceworld.org/ssa/bssa/article/71/6/2071/102118/the-character-of-high-frequency-strong-ground">https://pubs.geoscienceworld.org/ssa/bssa/article/71/6/2071/102118/the-character-of-high-frequency-strong-ground</url> ). Arias intensity records out to 100‐km yield stable stress drops for moderate‐to‐large magnitude earthquakes, M 6.5+; for smaller events ~ M 4.5–6.5, only closer‐in records yield stable results. For the 116 events considered, stress drops are about 35% larger for class 1 mainshocks than for traditional on‐fault class 2 aftershocks, and smaller for those aftershocks close to the main fault plane. Aftershock stress drops show large variability, however, implying that on average they rerupture weakened patches but can also rupture intact rock or high‐stress asperities. We observe an increase of stress drop with earthquake depth similar to that of other studies but do not find any significant faulting mechanism dependence. The variability of the Arias intensity‐based stress drop is lower than that of eGf‐based stress drops from Baltay et al. (2010, <url href="https://doi.org/10.1029/2009JB006736">https://doi.org/10.1029/2009JB006736</url> ; 2011, <url href="https://doi.org/10.1029/2011GL046698">https://doi.or </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> >我们决定了从NGA-West2的Arias强度数据库直接掉落的地震压力。 Arias强度（Arias，1970，<url href =“https://www.osti.gov/biblio/4167721”> https://www.osti.gov/biblio/4167721 </ url>）是一种成比例的工程测量在信号的显着持续时间内增加加速度的加速度的绝对值的积分。因此，它与根均线加速度密切相关，并且可以容易地连接到地震应力下降（Hanks＆amp; McGuire，1981，<URL Href =“https://pubs.geoscietyworld.org/ssa/bssa/article/ 71 / 6/2071 / 102118 / - 高频强 - 地面“> https://pubs.geoscietyworld.org/ssa/bssa/article/71/6/2071/102118/tho -of高频 - 强 - 地面</ URL>）。 Arias强度记录为100km的稳定应力下降，适度到大小的大地震，<B> M </ B> 6.5+;对于较小的事件〜 m </ b> 4.5-6.5，只有更近的记录产生稳定的结果。对于第116个事件，对于第1类主轴的应力下降比传统的故障级2余震更大，并且对于靠近主故障平面的余震较小，更小。然而，余震压力下降显示出大的变化意味着平均而平均削弱削弱削弱的斑块，但也可以破裂完整的岩石或高应力的粗糙度。我们观察到与其他研究的地震深度的压力下降增加，但没有发现任何显着的错误机制依赖。基于Arias强度的应力下降的可变性低于Baltay等人的基于EGF的应力下降的变化。（2010，<url href =“https://do.org/10.1029/2009jb006736”> https://doi.org/10.1029/2009JB006736 </ URL>; 2011，<URL HREF =“HTTPS：// DOI。 ORG / 10.1029 / 2011GL046698“> HTTPS：//DOI.OR </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>2019年第4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=Baltay Annemarie S.&option=202" target="_blank" rel="nofollow">Baltay Annemarie S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hanks Thomas C.&option=202" target="_blank" rel="nofollow">Hanks Thomas C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abrahamson Norman A.&option=202" target="_blank" rel="nofollow">Abrahamson Norman A.;</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 CA USA;</p> <p>USGSMenlo Park CA USA;</p> <p>Department of Civil and Environmental EngineeringUniversity of California BerkeleyBerkeley 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=earthquake stress drop&option=203" rel="nofollow">earthquake stress drop;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake ground motion&option=203" rel="nofollow">earthquake ground motion;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arias intensity&option=203" rel="nofollow">Arias intensity;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake source parameters&option=203" rel="nofollow">earthquake source parameters;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=attenuation&option=203" rel="nofollow">attenuation;</a> </p> <div class="translation"> 机译：地震应力下降;地震地面运动;arias强度;地震源参数;衰减; </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/0704025591754.html">Earthquake Stress Drop and Arias Intensity</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Baltay Annemarie S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Baltay Annemarie S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hanks Thomas C.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hanks Thomas C.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Abrahamson Norman A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Abrahamson Norman A. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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