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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Frictional Properties of Subduction Input Sediments at an Erosive Convergent Continental Margin and Related Controls on Décollement Slip Modes: The Costa Rica Seismogenesis Project
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Frictional Properties of Subduction Input Sediments at an Erosive Convergent Continental Margin and Related Controls on Décollement Slip Modes: The Costa Rica Seismogenesis Project

机译：渗透收敛大陆边缘胶片输入沉积物的摩擦性质及Décollement滑动模式下的相关控制：哥斯达黎加地震生成项目

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Abstract > The spectrum of slip modes occurring along shallow portions of the plate boundary décollement in subduction zones includes aseismic slip, slow slip, and seismogenic slip. The factors that control slip modes directly influence the hazard potential of subduction zones for generating large‐magnitude earthquakes and tsunamis. We conducted an experimental study of the frictional behavior of subduction input sediments, recovered from two Integrated Ocean Drilling Program expeditions to the erosive subduction margin offshore Costa Rica (Expeditions 334 and 344), employing rotary shear under hydrothermal conditions. The velocity dependence of friction was explored, using simulated gouges prepared from all major lithologies, covering a wide range of conditions representative for the initial stages of subduction. Temperature, effective normal stress, and pore fluid pressure were varied systematically up to 140?°C, 110 MPa, and 120 MPa, respectively. Sliding velocities up to 100 <fi>μ</fi> m/s, relevant for earthquake rupture nucleation and slow slip, were investigated. The only sediment type that produced frictional instabilities (i.e., laboratory earthquakes) was the calcareous ooze carried by the incoming Cocos Plate, which by virtue of its slip‐weakening behavior is also a likely candidate for triggering slow slip events. We evaluate this mechanism of producing unstable slip and consider alternatives. Therefore, locking and unlocking of plate boundary megathrusts are not only related to variations in pore fluid pressure but may also depend on the presence of pelagic carbonate‐rich lithologies. Subduction systems containing such input are likely low latitude, where extensive deposition of carbonates takes place above the carbonate compensation depth. </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 =“JGRB52978-ABS-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> >沿浅扫描发生的滑动模式频谱俯冲区域的板边界中的部分界限包括抗震滑动，慢速滑动和发震滑动。控制滑移模式直接影响俯冲区的灾害潜力，以产生大幅度地震和海啸。我们对俯冲投入沉积物的摩擦行为进行了实验研究，从两种综合海洋钻井计划探险中恢复到糜烂郊区欧洲肋斯塔RICA（探险334和344），在水热条件下采用旋转剪切。探索摩擦的速度依赖性，采用由所有主要岩性制备的模拟凿子，覆盖各种胶片初始阶段的各种条件。温度，有效的正常应力和孔隙流体压力分别在系统上系统地变化，分别为140℃，110MPa和120MPa。调查了与地震破裂成核和慢速滑动相关的100 <FI>μ</ Fi> M / s的滑动速度。产生摩擦稳定性（即实验室地震）的唯一沉积物是进入的Cocos板携带的钙质渗纹，其借助于其滑动弱化行为也是触发慢速滑动事件的可能候选者。我们评估了这种生产不稳定滑动的机制，考虑替代品。因此，锁定和解锁板边界巨大不仅与孔隙流体压力变化有关，而且还可以取决于富含碳酸酯的岩石的存在。含有这种输入的俯冲系统很可能是低纬度，其中碳酸盐的广泛沉积发生在碳酸盐补偿深度之上。 </ 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-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24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=Kurzawski Robert Marek&option=202" target="_blank" rel="nofollow">Kurzawski Robert Marek;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niemeijer André Rik&option=202" target="_blank" rel="nofollow">Niemeijer André Rik;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stipp Michael&option=202" target="_blank" rel="nofollow">Stipp Michael;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Charpentier Delphine&option=202" target="_blank" rel="nofollow">Charpentier Delphine;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Behrmann Jan Hinrich&option=202" target="_blank" rel="nofollow">Behrmann Jan Hinrich;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Spiers Christopher James&option=202" target="_blank" rel="nofollow">Spiers Christopher James;</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>GEOMAR Helmholtz Centre for Ozean Research KielKiel Germany;</p> <p>HPT LaboratoryUtrecht UniversityUtrecht Netherlands;</p> <p>Institute of GeologyUniversity of InnsbruckInnsbruck Austria;</p> <p>Université de Franche‐ComtéBesancon France;</p> <p>GEOMAR Helmholtz Centre for Ozean Research KielKiel Germany;</p> <p>HPT LaboratoryUtrecht UniversityUtrecht Netherlands;</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=Frictional controls on shallow subduction channel deformation&option=203" rel="nofollow">Frictional controls on shallow subduction channel deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=shallow seismogenesis and generation of slow earthquakes in an erosive system&option=203" rel="nofollow">shallow seismogenesis and generation of slow earthquakes in an erosive system;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Costa Rica Seismogenesis Project (CRISP)&option=203" rel="nofollow">Costa Rica Seismogenesis Project (CRISP);</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=IODP expeditions 334 and 344&option=203" rel="nofollow">IODP expeditions 334 and 344;</a> </p> <div class="translation"> 机译：浅层俯冲通道变形的摩擦控制;浅地发生和腐蚀系统中慢地震的产生;哥斯达黎加地区生成项目（清脆）;IODP探险334和344; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591069.html">Frictional Properties of Subduction Input Sediments at an Erosive Convergent Continental Margin and Related Controls on Décollement Slip Modes: The Costa Rica Seismogenesis Project</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kurzawski Robert Marek&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kurzawski Robert Marek,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niemeijer André Rik&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Niemeijer André Rik,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stipp Michael&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Stipp Michael,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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