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Stratigraphic Control of Frontal Décollement Level and Structural Vergence and Implications for Tsunamigenic Earthquake Hazard in Sumatra, Indonesia

机译：普遍地来的地层控制与苏门答腊州苏门答腊州苏庇地震危害的结构性与结构性效果及其影响

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Abstract > Propagation of fault rupture to the seafloor is a likely cause of enhanced tsunami generation during megathrust earthquakes. New, high‐resolution seismic reflection profiles and swath bathymetry collected across the northern limit of the M <sub> w </sub> 7.8, 25 October 2010 Mentawai tsunami earthquake rupture reveal significant and systematic lateral variations in both the stratigraphic level of the frontal Sunda megathrust and the vergence of its frontal ramp faults. Where ramp faults are uniformly seaward vergent, the décollement resides on top of a strong reflector marking the inferred top of pelagic sediments. Where ramp faults are bivergent (both landward and seaward), the décollement is localized within the subducting clastic sequence, above a xseismically transparent unit inferred to be distal fan muds. Where ramp faults are uniformly landward vergent, the décollement is directly on top of the oceanic crust of the subducting Investigator Fracture Zone. Enhanced surface uplift and tsunamigenesis during the 2010 tsunamigenic earthquake appear to have coincided with propagation of rupture into frontal areas with well‐developed structural bivergence. Frontal bivergence is a geological signal of low basal traction during accrual of slip, and offshore of Sumatra this structural style may mark areas of enhanced tsunami hazard posed by small‐magnitude, shallow megathrust ruptures that propagate into the incoming terrigenous sequence at near‐trench levels. </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> > 故障破裂对海底的传播是巨大地震期间增强海啸发电的可能原因。新的，高分辨率的地震反射曲线和北极极限收集的SWATH浴室 m </ i> <sub> w </ i> </ sub> 7.8，2010年10月25日芯瓦海啸地震破裂揭示了额外巨大巨大的地层水平和额叶故障的折射的显着和系统的横向变化。如果斜坡故障均匀的海向验证，则塞加尔蒙在强力反射器顶部标记了翻译后的沉积物的推断顶部。如果斜坡故障伴有（陆地和海洋），则塞克莱姆在桥面碎片序列内定位，上方被推断为远端风扇泥浆。如果斜坡故障均匀地陆地验证，则Décollement直接位于底壳调查仪骨折区的海洋地壳之上。 2010年Tsunamigenic地震期间增强的表面隆起和啸叫率似乎恰逢破裂传播到具有良好发展的结构性发育的前地区。正面疾病是在近沟壑区的沉淀下的可应计过程中的低基础牵引的地质信号，而苏门答腊的近海可能标志着增强的海啸危险，浅巨大破裂，在近沟渠水平宣传到进入的植入序列中。 。 </ 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3期</span><b style="margin: 0 2px;">|</b><span>共19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=Bradley Kyle&option=202" target="_blank" rel="nofollow">Bradley Kyle;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qin Yanfang&option=202" target="_blank" rel="nofollow">Qin Yanfang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Carton Hélène&option=202" target="_blank" rel="nofollow">Carton Hélène;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hananto Nugroho&option=202" target="_blank" rel="nofollow">Hananto Nugroho;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Villanueva‐Robles Fernando&option=202" target="_blank" rel="nofollow">Villanueva‐Robles Fernando;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Leclerc Fréderique&option=202" target="_blank" rel="nofollow">Leclerc Fréderique;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shengji Wei&option=202" target="_blank" rel="nofollow">Shengji Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tapponier Paul&option=202" target="_blank" rel="nofollow">Tapponier Paul;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sieh Kerry&option=202" target="_blank" rel="nofollow">Sieh Kerry;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Singh Satish&option=202" target="_blank" rel="nofollow">Singh Satish;</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>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Equipe de Géosciences Marines Institut de Physique du Globe de Paris (CNRS Paris Diderot Sorbonne Paris Cité)Paris France;</p> <p>Equipe de Géosciences Marines Institut de Physique du Globe de Paris (CNRS Paris Diderot Sorbonne Paris Cité)Paris France;</p> <p>Now at Research Center for Deep SeaIndonesian Institute of SciencesAmbon Maluku Indonesia;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Géoazur Université Nice Sophia Antipolis (Université C?te d'Azur CNRS IRD Observatoire de la C?te d'Azur)Valbonne France;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</p> <p>Earth Observatory of SingaporeNanyang Technological UniversitySingapore;</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=subduction&option=203" rel="nofollow">subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tsunami&option=203" rel="nofollow">tsunami;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=megathrust&option=203" rel="nofollow">megathrust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sumatra&option=203" rel="nofollow">Sumatra;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Indian Ocean&option=203" rel="nofollow">Indian Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sunda&option=203" rel="nofollow">Sunda;</a> </p> <div class="translation"> 机译：俯冲;海啸;巨大的;苏门答腊;印度洋;孙丹人; </div> </li> 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2012</span><span>,第006期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-jilin-university-earth-science-edition_thesis/0201293910249.html">2000年苏门答腊M_S8.0地震对缅甸M_S6.5地震动态应力触发作用及影响因素</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=张彬&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张彬</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=陆远忠&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,陆远忠</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘耀炜&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘耀炜</a> <span> <a href="/journal-cn-50284/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 吉林大学学报：地球科学版 </a> </span> <span> . 2012</span><span>,第S2期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" 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