Eclogitization of the Subducted Oceanic Crust and Its Implications for the Mechanism of Slow Earthquakes

Wang Xinyang; Zhao Dapeng; Suzuki Haruhiko; Li Jiabiao; Ruan Aiguo

摘要

Abstract > The generating mechanism and process of slow earthquakes can help us to better understand the seismogenic process and the petrological evolution of the subduction system, but they are still not very clear. In this work we present robust <fi>P</fi> and <fi>S</fi> wave tomography and Poisson's ratio images of the subducting Philippine Sea Plate beneath the Kii peninsula in Southwest Japan. Our results clearly reveal the spatial extent and variation of a low‐velocity and high Poisson's ratio layer which is interpreted as the remnant of the subducted oceanic crust. The low‐velocity layer disappears at depths 50?km, which is attributed to crustal eclogitization and consumption of fluids. The crustal eclogitization and destruction of the impermeable seal play a key role in the generation of slow earthquakes. The Moho depth of the overlying plate is an important factor affecting the depth range of slow earthquakes in warm subduction zones due to the transition of interface permeability from low to high there. The possible mechanism of the deep slow earthquakes is the dehydrated oceanic crustal rupture and shear slip at the transition zone in response to the crustal eclogitization and the temporal stress/strain field. A potential cause of the slow event gap existing beneath easternmost Shikoku and the Kii channel is the premature rupture of the subducted oceanic crust due to the large tensional force. </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> >慢地震的发电机制和过程可以帮助我们更好地了解发泻过程和俯冲系统的岩石学演变，但它们仍然不是很清楚。在这项工作中，我们呈现强大的<fi> p </ fi>波断层扫描和泊松比例的菲律宾海底在日本西南部的猕猴桃水下底板的比例。我们的结果清楚地揭示了低速度和高泊松比例的空间范围和变化，其被解释为后果海外壳的残余物。低速层在深度和gt中消失了50 km，这归因于地壳eNlogitization和流体的消耗。不透水密封的地壳eClogitization和破坏在慢地震的产生中起着关键作用。覆盖板的Moho深度是影响温暖俯冲区域中缓慢地震深度范围的重要因素，由于界面渗透率从低到高于那里的过渡。深缓慢地震的可能机制是过渡区的脱水海洋地壳破裂和剪切滑动响应地壳eClogitization和时间应力/应变场。最大的Shikoku下面存在缓慢事件差距的潜在原因，并且由于大规模的张力而发生过滤的海洋地壳过早破裂。 </ p> </ abstract> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第24期</span><b style="margin: 0 2px;">|</b><span>共8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=Wang Xinyang&option=202" target="_blank" rel="nofollow">Wang Xinyang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Dapeng&option=202" target="_blank" rel="nofollow">Zhao Dapeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Suzuki Haruhiko&option=202" target="_blank" rel="nofollow">Suzuki Haruhiko;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Jiabiao&option=202" target="_blank" rel="nofollow">Li Jiabiao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ruan Aiguo&option=202" target="_blank" rel="nofollow">Ruan Aiguo;</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>Collaborative Innovation Center of South China Sea Studies and School of Geographic and Oceanographic SciencesNanjing UniversityNanjing China;</p> <p>Department of GeophysicsTohoku UniversitySendai Japan;</p> <p>Earthquake Research CenterOyo CorporationTokyo Japan;</p> <p>Second Institute of OceanographyState Oceanic AdministrationHangzhou China;</p> <p>Second Institute of OceanographyState Oceanic AdministrationHangzhou China;</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 earthquakes&option=203" rel="nofollow">slow earthquakes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal eclogitization&option=203" rel="nofollow">crustal eclogitization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tomography&option=203" rel="nofollow">tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction dynamics&option=203" rel="nofollow">subduction dynamics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=permeability&option=203" rel="nofollow">permeability;</a> </p> <div class="translation"> 机译：慢地震;地壳eclogitization;断层扫描;俯冲动态;渗透率; 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A.Witze</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=生冬梅&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,生冬梅</a> <span> <a href="/journal-cn-5012/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 世界地震译丛 </a> </span> <span> . 2018</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_seismology-geology_thesis/0201253222700.html">汶川地震后中下地壳及上地幔的粘弹性效应引起的应力变化与芦山地震的发生机制</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=雷兴林&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 雷兴林</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=马胜利&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,马胜利</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=苏金蓉&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,苏金蓉</a> <span> <a href="/journal-cn-4916/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震地质 </a> </span> <span> . 2013</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-geodesy-geodynamics_thesis/0201252724038.html">地壳分层和地壳厚度对汶川地震同震效应的影响</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=谈洪波&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 谈洪波</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=申重阳&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,申重阳</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=玄松柏&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,玄松柏</a> <span> <a href="/journal-cn-4886/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 大地测量与地球动力学 </a> </span> <span> . 2010</span><span>,第004期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_crustal-structure-stress_thesis/0201267054015.html">地壳应力,地壳应力变化和地壳变动：周期性地壳变动与地震活动的交…</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=田中丰&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 田中丰</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=祁英男&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,祁英男</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> . 1996</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_china-earthquake-engineering-journal_thesis/0201254347362.html">地形变场与现代地壳垂直运动及地震活动关系初探(Ⅱ)--地凸凹区与地壳运动及地震活动的关系</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭维栋&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郭维栋</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=汤懋苍&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,汤懋苍</a> <span> <a href="/journal-cn-5027/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 地震工程学报 </a> </span> <span> . 2003</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-9975_thesis/020222360323.html">塌陷地震与地壳深部水循环的关系初探</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Jiansheng&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . Chen Jiansheng</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陈建生&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陈建生</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" class="tuijian_auth tuijian_authcolor">,Liu Zhen</a> <span> <a href="/conference-cn-9975/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 第九届中国水论坛 </a> <span> <span> . 2011</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/0203151245.html">地震定位对剪切波分裂的影响分析与张家口-渤海地震带西端地壳介质各向异性</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵博&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵博</a> <span> . 2010</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" 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href="/patent-detail/06130403085724.html">METHOD FOR FORMING AND APPLICATION OF GLOBAL RADIOHYDROACOUSTIC SYSTEM OF MONITORING ATMOSPHERIC, OCEANIC AND CRUSTAL FIELDS IN MARINE ENVIRONMENT AND RECOGNITION OF SOURCES THEREOF</a> <b>[P]</b> . <span> 外国专利：  RU2017130991A3 </span> <span> . 2019-03-01</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：海洋环境中大气，海洋和地壳监测的全球放射性水声系统的形成和应用方法及其资源识别 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130408477458.html">ACOUSTIC TOMOGRAPHY SYSTEM FIELDS IN THE ATMOSPHERE, THE OCEANS AND CRUST OF DIFFERENT PHYSICAL NATURE IN THE MARINE ENVIRONMENT</a> <b>[P]</b> . <span> 外国专利：  RU2624602C1 </span> <span> . 2017-07-04</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> 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