Cascadia Onshore‐Offshore Site Response, Submarine Sediment Mobilization, and Earthquake Recurrence

机译：Cascadia Onshore-Offshore网站反应，潜艇沉积物动员和地震复发

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Abstract > Local geologic structure and topography may modify arriving seismic waves. This inherent variation in shaking, or “site response,” may affect the distribution of slope failures and redistribution of submarine sediments. I used seafloor seismic data from the 2011 to 2015 Cascadia Initiative and permanent onshore seismic networks to derive estimates of site response, denoted <fi>S</fi> <sub> <fi>n</fi> </sub> , in low‐ and high‐frequency (0.02–1 and 1–10?Hz) passbands. For three shaking metrics (peak velocity and acceleration and energy density) <fi>S</fi> <sub> <fi>n</fi> </sub> varies similarly throughout Cascadia and changes primarily in the direction of convergence, roughly east‐west. In the two passbands, <fi>S</fi> <sub> <fi>n</fi> </sub> patterns offshore are nearly opposite and range over an order of magnitude or more across Cascadia. <fi>S</fi> <sub> <fi>n</fi> </sub> patterns broadly may be attributed to sediment resonance and attenuation. This and an abrupt step in the east‐west trend of <fi>S</fi> <sub> <fi>n</fi> </sub> suggest that changes in topography and structure at the edge of the continental margin significantly impact shaking. These patterns also correlate with gravity lows diagnostic of marginal basins and methane plumes channeled within shelf‐bounding faults. Offshore <fi>S</fi> <sub> <fi>n</fi> </sub> exceeds that onshore in both passbands, and the steepest slopes and shelf coincide with the relatively greatest and smallest <fi>S</fi> <sub> <fi>n</fi> </sub> estimates at low and high frequencies, respectively; the </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> >本地地质结构和地形可能修改到达地震波。这种固有的摇动或“站点反应”的变化可能会影响斜坡故障的分布和潜艇沉积物的重新分配。我使用2011年至2015年Cascadia主动和永久陆上地震网络的海底地震数据，以推导出现场响应的估计，表示<fi> s </ fi> <sub> <fi> n </ fi> </ sub>低频和高频（0.02-1和1-10？Hz）通带。对于三个振动度量（峰值速度和加速度和能量密度）<fi> s </ fi> <sub> <fi> n </ fi> </ sub>在整个Cascadia中同样不同，并且主要在收敛方向上变化，大致东西。在两个通带中，<fi> s </ fi> <sub> <fi> n </ fi> </ sub>模式近海几乎相反，范围超过Cascadia的数量级或更多。 <fi> s </ fi> <fi> n </ fi> </ sub>图案广泛可能归因于沉积物共振和衰减。 <fi> s </ fi> <sub> <fi> </ fi> </ sub的东西趋势的突然阶跃趋势呈现出大陆边缘边缘的地形和结构的变化冲击摇动。这些图案也与重力低点相关的边缘盆地和甲烷羽毛在搁板限制故障内引起的。离岸<fi> s </ fi> <sub> <fi> n </ fi> </ sub>超过通行带中的陆上，最陡峭的斜坡和架子与相对较大，最小的<fi> s </ she fi> <sub> <fi> n </ sub> </ sub>在低频和高频下估计;这 </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2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=Gomberg J.&option=202" target="_blank" rel="nofollow">Gomberg J.;</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>U.S. Geological SurveyUniversity of WashingtonSeattle WA 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=Site response&option=203" rel="nofollow">Site response;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sediment mobilization&option=203" rel="nofollow">sediment mobilization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake recurrence&option=203" rel="nofollow">earthquake recurrence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=turbidite&option=203" rel="nofollow">turbidite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=slope failure&option=203" rel="nofollow">slope failure;</a> </p> <div class="translation"> 机译：网站响应;沉积物动员;地震复发;浊度;斜坡故障; </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/0704025592778.html">Cascadia Onshore‐Offshore Site Response, Submarine Sediment Mobilization, and Earthquake Recurrence</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gomberg J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gomberg J. </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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