Localized Slip and Associated Fluidized Structures Record Seismic Slip in Clay‐Rich Fault Gouge

机译：局部滑动和相关的流化结构记录富含粘土故障凿岩的地震滑动

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Abstract >Fault rocks can weaken dramatically with increasing slip rate, which results in localization of slip and earthquakes. Exhumed fault zones and fault rocks deformed at seismic rates in the laboratory both show that deformation can become extremely localized to zones less than or equal to millimeters thick. However, localization can occur during aseismic slip, so evidence of localization cannot necessarily be interpreted as having occurred coseismically. Dynamic weakening that occurs during earthquakes is the result of processes that are unique to seismic slip rates, and previous results from carbonates show that these processes produce unique microstructures. We evaluate whether coseismic deformation at low normal stress produces unique structures within the localized slip zones and adjacent gouge that develop in clay‐rich gouge from the Central Deforming Zone of the San Andreas fault. We measured the thickness and orientations of localized slip zones and their internal lamina, particle orientations, and particle size distributions of gouge sheared from 0.35 to 1.3?m/s velocity, up to 25‐m displacement, and 1‐MPa normal stress, under water‐wet and room‐dry conditions. We find that the thicknesses of localized slip zones and their internal laminae are consistent with numerical formulations for thermal pressurization in wet gouge and both thermal decomposition and cataclastic deformation in dry gouge. Localized zones form coincident with a zone of fluidized gouge that accommodates at most 10% of the shear strain. We conclude that the combined occurrence of foliated localized shear zones with a zone of fluidized gouge may provide a record of seismicity in clay‐rich gouges. </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 =“JGRB53069-ABS-ABS-0001”> <标题类型=“MAIN”> Abstract </ Title> <P>故障摇滚可以随着较高的滑动逐渐减弱速率，导致滑动和地震的本地化。挖掘出故障区和故障岩石在实验室中的地震速率变形，两者都表明，变形可以极大地定位到小于或等于毫米厚的区域。然而，在抗遍滑动期间可以发生定位，因此本地化证据不一定被解释为已发生电动发电机。地震期间发生的动态弱化是对地震滑动率独特的过程的结果，碳酸盐的先前结果表明这些过程产生独特的微观结构。我们评估低正常应力下的电影变形是否在局部滑动区和邻近凿孔中产生独特的结构，这些结构从San Andreas故障的中央变形区域开发富含粘土的凿孔。我们测量了局部滑动区的厚度和方向及其内部薄层，颗粒取向和粒度分布从0.35至1.3Ω·m / s速度剪切，高达25米的位移和1-MPa正常应力水湿和室温条件。我们发现局部滑动区及其内部薄片的厚度与湿凿中的热加压的数值配方一致，以及干凿中的热分解和热分解变形。局部区域形式与流化凿孔区域重合，该区域适应最多10％的剪切应变。我们得出结论，叶片局部剪切区的结合发生在流化凿区中可以提供富含粘土的凿地性的地震记录。</ 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>2018年第10期</span><b style="margin: 0 2px;">|</b><span>共21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=French Melodie E.&option=202" target="_blank" rel="nofollow">French Melodie E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chester Judith S.&option=202" target="_blank" rel="nofollow">Chester Judith 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 Environmental and Planetary SciencesWilliam Marsh Rice UniversityHouston TX USA;</p> <p>Department of Geology and Geophysics Center for TectonophysicsTexas A&</p> <p>M UniversityCollege Station TX 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;"> </p> </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/0704025592314.html">Localized Slip and Associated Fluidized Structures Record Seismic Slip in Clay‐Rich Fault Gouge</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=French Melodie E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">French Melodie E.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chester Judith S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chester Judith S. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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