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Investigating Segmentation in Cascadia: Anisotropic Crustal Structure and Mantle Wedge Serpentinization from Receiver Functions

机译:Cascadia的调查分割:来自接收器功能的各向异性地壳结构和地幔楔形蛇形化

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Abstract >The Cascadia subduction zone exhibits along‐strike segmentation in structure, processes, and seismogenic behavior. While characterization of seismic anisotropy can constrain deformation processes at depth, the character of seismic anisotropy in Cascadia remains poorly understood. This is primarily due to a lack of seismicity in the subducting Juan de Fuca slab, which limits shear wave splitting and other seismological analyses that interrogate the fine‐scale anisotropic structure of the crust and mantle wedge. We investigate lower crustal anisotropy and mantle wedge structure by computing P‐to‐S receiver functions at 12 broadband seismic stations along the Cascadia subduction zone. We observe P‐to‐SV converted energy consistent with previously estimated Moho depths. Several stations exhibit evidence of an “inverted Moho” (i.e., a downward velocity decrease across the crust‐mantle boundary), indicative of a serpentinized mantle wedge. Stations with an underlying hydrated mantle wedge appear prevalent from northern Washington to central Oregon, but sparse in southern Oregon and northern California. Transverse component receiver functions are complex, suggesting anisotropic and/or dipping crustal structure. To constrain the orientation of crustal anisotropy we compute synthetic receiver functions using manual forward modeling. We determine that the lower crust shows variable orientations of anisotropy along‐strike, with highly complex anisotropy in northern Cascadia, and generally NW‐SE and NE‐SW orientations of slow‐axis anisotropy in central and southern Cascadia, respectively. The orientations of anisotropy from this work generally agree with those inferred from shear wave splitting of tremor studies at similar locations, lending confidence to this relatively new method of inferring seismic anisotropy from slow earthquakes. </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”> <标题类型=“main”>抽象</ title> > Cascadia俯冲区沿着结构,过程和发作行为沿着打击分段展示。虽然地震各向异性的表征可以在深度限制变形过程的同时,Cascadia中地震各向异性的特征仍然明确。这主要是由于化脓性Juan de Fuca板块缺乏地震性,这限制了剪切波分裂和其他地震学分析,以询问地壳和地幔楔的微级各向异性结构。我们通过在沿着Cascadia俯冲区的12个宽带地震站计算P-To-S接收器功能来研究较低的地壳各向异性和地幔楔形结构。我们观察与先前估计的Moho深度一致的p-to-sv转换能量。几个站表现出“倒置的moho”的证据(即,横跨外壳边界的向下速度下降),指示蛇形的地幔楔形物。带有底层水合的地幔楔的电台从华盛顿北部到俄勒冈州中部,但在俄勒冈州和北加州稀疏。横向部件接收器功能复杂,暗示各向异性和/或浸渍地壳结构。为了限制地壳各向异性的方向,我们使用手动前向建模计算合成接收器功能。我们确定下面地壳显示各向异性的可变取向沿着剧烈的各向异性,在北部的北部各向异性中具有高度复杂的各向异性,以及中央和南部的Cascadia中的慢轴各向异性的NW-SE和NE-SW定位。来自这项工作的各向异性的方向通常与在类似地点的震颤研究的剪切波分裂推断的那些,对这种相对较新的方法从缓慢地震中推断出地震各向异性的相对较新的方法。</ 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>2017年第10期</span><b style="margin: 0 2px;">|</b><span>共16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=Krueger Hannah E.&option=202" target="_blank" rel="nofollow">Krueger Hannah E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wirth Erin A.&option=202" target="_blank" rel="nofollow">Wirth Erin A.;</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>Department of Geological and Environmental SciencesAppalachian State UniversityBoone NC USA;</p> <p>Department of Earth and Space SciencesUniversity 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=Cascadia&option=203" rel="nofollow">Cascadia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=subduction zone&option=203" rel="nofollow">subduction zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic anisotropy&option=203" rel="nofollow">seismic anisotropy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=serpentinization&option=203" rel="nofollow">serpentinization;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=receiver functions&option=203" rel="nofollow">receiver functions;</a> </p> <div class="translation"> 机译:Cascadia;俯冲区;地震各向异性;蛇形化;接收器功能; </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/0704023360458.html">Investigating Segmentation in Cascadia: Anisotropic Crustal Structure and Mantle Wedge Serpentinization from Receiver Functions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krueger Hannah E.&option=202" 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