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首页> 外文期刊>Geochemistry, geophysics, geosystems >Slow‐Slip Recurrent Pattern Changes: Perturbation Responding and Possible Scenarios of Precursor toward a Megathrust Earthquake
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Slow‐Slip Recurrent Pattern Changes: Perturbation Responding and Possible Scenarios of Precursor toward a Megathrust Earthquake

机译:缓冲复发模式改变:扰动响应和可能对巨大地震的前兆的情况

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摘要

Abstract >Advances in geodetic techniques enable us to detect “slow‐earthquake” transients (e.g., slow‐slip events, SSEs) with improving accuracy and coverage. Recent observations reveal intriguing changes of SSE behavior before and/or after earthquakes. However, the physics behind these observations remain largely unknown. How does SSE pattern change during megathrust earthquake super‐cycle? How do SSEs respond to “external” tectonic perturbations such as stress perturbation from earthquakes, or nontectonic forces such as tidal modulation and seasonal loading? Can SSE pattern changes shed light on the onset of a large earthquake? To address these questions, we employ laboratory‐based rate‐and‐state frictional law on subduction zone faults with realistic frictional properties incorporating megathrust earthquake and SSE regions. We conduct 2‐D/3‐D quasi‐dynamic earthquake cycle simulations to study the “intrinsic” SSE pattern changes as how it evolves at different stages of the earthquake cycle, versus the changes in SSE pattern responding to external stress perturbations. Our results suggest that, despite both intrinsic and perturbation models are capable to introduce large variability in SSE pattern, there are considerable observable characteristics that can be used to differentiate these two models. Without external perturbation the SSE patterns change intrinsically during the super‐cycle. The recurrence interval and peak slip rate of SSEs decrease significantly right before megathrust earthquake and could be used as a potential warning sign. Whereas SSE patterns can vary significantly when perturbed by an earthquake or other tectonic/nontectonic sources. Recurring SSEs can be advanced or delayed by external perturbations, and multiple SSEs can be affected if perturbation is long‐lasting. </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”> <标题类型=“main”>抽象</ title> >大地测量技术的进步使我们能够通过提高准确性和覆盖率来检测“慢地震”瞬态(例如,慢速速度事件,SSE)。最近的观察结果揭示了地震前和/或后/或后/或后/或后/或之后的兴趣变化。然而,这些观察结果背后的物理仍然很大程度上是未知的。 SSE模式如何在巨大的地震超级周期内改变? SSE如何应对“外部”构造扰动,例如地震的压力扰动,或诸如潮汐调制和季节性装载的局部力量? SSE模式是否会改变大地震发生的闪光灯?为了解决这些问题,我们采用实验室的汇率和国家摩擦法在俯冲区断层上,采用巨大的摩擦物质,融合了巨大的地震和上级地区。我们进行2-D / 3-D准动态地震循环模拟,以研究“内在”的SSE模式改变,以及如何在地震周期的不同阶段演变,与外部压力扰动的SSE模式的变化相比。我们的研究结果表明,尽管既有内在和扰动模型都能够在SSE模式下引入大的可变性,但是可以使用相当大的可观察特性来区分这两个模型。如果没有外部扰动,SSE模式在超周期内的本质上变化。在Megathrust地震之前,SSE的复发间隔和峰值滑移率明显减少,可以用作潜在的警告标志。当由地震或其他构造/义源源扰乱时,虽然SSE模式可以显着变化。经常性SSE可以通过外部扰动提前或延迟,如果扰动持久,则可能会影响多个SSES。</ 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-23285/'>《Geochemistry, geophysics, geosystems》</a> <b style="margin: 0 2px;">|</b><span>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共20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=Luo Yingdi&option=202" target="_blank" rel="nofollow">Luo Yingdi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Zhen&option=202" target="_blank" rel="nofollow">Liu Zhen;</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>Jet Propulsion LaboratoryPasadena CA USA;</p> <p>Jet Propulsion LaboratoryPasadena 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=slow‐slip event&option=203" rel="nofollow">slow‐slip event;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=rate‐and‐state friction&option=203" rel="nofollow">rate‐and‐state friction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction model&option=203" rel="nofollow">subduction model;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mega thrust earthquake&option=203" rel="nofollow">mega thrust earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=stress perturbation&option=203" rel="nofollow">stress perturbation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake prediction&option=203" rel="nofollow">earthquake prediction;</a> </p> <div class="translation"> 机译:慢速比赛;速率和状态摩擦;俯冲模型;兆推力地震;压力扰动;地震预测; 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