A Physical Model for Interseismic Erosion of Locked Fault Asperities

机译：锁定故障抑制措施苦易侵蚀的物理模型

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Abstract >The conventional “asperity model” posits that faults are partitioned into fixed velocity‐weakening (VW) patches (asperities) that are locked interseismically and velocity‐strengthening (VS) regions that creep stably without accumulating stress. However, studies of GPS‐derived deformation in northern Japan have shown that interseismic strain in the Tohoku region did not accumulate at a constant rate (as expected) but gradually decreased from 1996 to 2011. This change in strain rate is consistent with locked asperities shrinking by ～75% in area during this period. Here we consider a modification to the conventional asperity model, such that thermal pressurization (TP) is active over an area that encompasses a VW region and part of the surrounding VS region. In our quasi‐dynamic simulations, TP causes shear stress during rapid slip to decrease to very low levels. During the interseismic period, stress gradually recovers to steady state friction at the plate rate, at which point stable creep initiates. The creep front propagates inward, effectively eroding the locked asperity. For uniform properties, the locked area shrinks roughly linearly in time through the VS region. Locked asperities shrink more slowly with higher nominal friction coefficient or background effective normal stress in the VS region, lower hydraulic diffusivity, and larger TP zones. Lateral heterogeneity in properties can give rise to nonlinear erosion. Predictions from this model can be compared against GPS data to test whether the model can explain the observed changes in interseismic strain rate in Tohoku. </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 =“JGRB52313-Abs-Abs-0001”> <标题类型=“main”>抽象</ title> >传统的“粗糙模型”Posits将故障分区为固定速度 - 脱落（VW）贴片（VW）贴片（粗糙度）锁定的速度和速度强化（VS）区域，其稳定地蠕变而不会累积应力。然而，日本北部GPS衍生变形的研究表明，东北地区的致力菌株并未以恒定的速率（如预期）累积（如预期），但从1996年至2011年逐渐下降。这种应变率的变化与锁定速度缩小一致在此期间面积〜75％。这里我们考虑对传统粗糙模型的修改，使得热加压（TP）在包含VW区域的区域和周围VS区域的一部分的区域上有效。在我们的准动态模拟中，TP在快速滑动期间导致剪切应力减小到极低水平。在造型期间，应力逐渐恢复到板率下的稳态摩擦，在该稳定蠕变引发点。蠕变前沿向内传播，有效地侵蚀锁定的粗糙度。对于均匀性，锁定区域通过VS区域大致缩小。锁定的粗糙度在VS区域，较低的液压扩散率和较大的TP区域中，较高的标称摩擦系数或背景有效正常应力缩短。性质中的横向异质性可以产生非线性侵蚀。可以将来自该模型的预测与GPS数据进行比较，以测试模型是否可以解释OHHOKU中的观察到的致力学应变率的变化。</ 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=Mavrommatis Andreas P.&option=202" target="_blank" rel="nofollow">Mavrommatis Andreas P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Segall Paul&option=202" target="_blank" rel="nofollow">Segall Paul;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Johnson Kaj M.&option=202" target="_blank" rel="nofollow">Johnson Kaj M.;</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 GeophysicsStanford UniversityStanford CA USA;</p> <p>Department of GeophysicsStanford UniversityStanford CA USA;</p> <p>Department of Earth and Atmospheric SciencesIndiana UniversityBloomington IN 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=Transient deformation&option=203" rel="nofollow">Transient deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Earthquake cycle&option=203" rel="nofollow">Earthquake cycle;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rate‐state friction&option=203" rel="nofollow">Rate‐state friction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fault mechanics&option=203" rel="nofollow">Fault mechanics;</a> </p> <div class="translation"> 机译：瞬态变形;地震循环;率 - 状态摩擦;故障力学; </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/0704020651390.html">A Physical Model for Interseismic Erosion of Locked Fault Asperities</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mavrommatis Andreas P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Mavrommatis Andreas P.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Segall Paul&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Segall Paul,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Johnson Kaj M.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Johnson Kaj M. </a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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href="/patent-detail/06130445720910.html">Diagnostics for recognition of fault models in a common ramp diesel injector commands, in which one or more fault symptoms are linked to a physical fault</a> <b>[P]</b> . <span> 外国专利：  FR2821161A1 </span> <span> . 2002-08-23</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：用于在常见的斜升柴油机喷油器命令中识别故障模型的诊断程序，其中一个或多个故障症状与物理故障相关 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130443684607.html">Method for predicting the effects of faults or interference occurring in a production system on production, involves using physical models to indicate a component failure and the effects of such a failure are then evaluated</a> <b>[P]</b> . <span> 外国专利：  DE10210565A1 </span> <span> . 2003-09-18</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: 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