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Seismic Imaging and Physical Properties of the Endeavour Segment: Evidence that Skew Between Mantle and Crustal Magmatic Systems Governs Spreading Center Processes

机译：努力分部的地震成像和物理性质：伴侣和地壳岩石系统之间歪斜的证据治理扩散中心过程

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Abstract > We invert Pg , PmP , and Pn traveltimes from an active‐source, multiscale tomography experiment to constrain the three‐dimensional isotropic and anisotropic P wave velocity structure of the topmost oceanic mantle and crust and crustal thickness variations beneath the entire Endeavour segment of the Juan de Fuca Ridge. The isotropic velocity structure is characterized by a semicontinuous, narrow (5‐km‐wide) crustal low‐velocity volume that tracks the sinuous ridge axis. Across the Moho, the low‐velocity volume abruptly broadens to approximately 20?km in width and displays a north‐south linear trend that connects the two overlapping spreading centers bounding the segment. From the seismic results, we estimate the thermal structure and melt distribution beneath the Endeavour segment. The thermal structure indicates that the observed skew, or lateral offset, between the crustal and mantle magmatic systems is a consequence of differences in mechanisms of heat transfer at crustal and mantle depths, with the crust and mantle dominated by advection and conduction, respectively. Melt volume estimates exhibit significant along‐axis variations that coincide with the observed skew between the mantle and crustal magmatic systems, with sites of enhanced crustal melt volumes and vigorous hydrothermal activity corresponding to regions where the mantle and crustal magmatic systems are vertically aligned. These results contradict models of ridge segmentation that predict enhanced and reduced melt supply beneath the segment center and ends, respectively. Our results instead support a model in which segment‐scale skew between the crustal and mantle magmatic systems governs magmatic and hydrothermal processes at mid‐ocean ridges. </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> > 我们倒了 pg </ i> 那 PMP </ i> ， 和 pn </ i> 来自主动源，多尺度断层扫描实验的旅行时间来限制三维各向同性和各向异性 p </ i> Juan de Fuca Ridge的整个努力段下面最顶层海洋地幔和地壳厚度变化的波速结构。各向同性速度结构的特征在于追踪致力脊轴的半连续窄（5公里）的地壳低速体积。在MOHO上，低速度突然宽度宽度宽度，宽度约为20千米，并显示南北线性趋势，连接横向段的两个重叠扩展中心。从地震结果中，我们估计在努力段下的热结构和熔体分布。热结构表明，在地壳和地幔岩石系统之间观察到的歪斜或横向偏移是在地壳和地幔深度的热传递机制的差异，分别由平流和传导主导地壳和地幔。熔体体积估计表现出显着的沿着轴上变化，其与地幔和地壳岩石系统之间观察到的倾斜相一致，具有增强的地壳熔体体积和对应于地幔和地壳岩石系统垂直对齐的区域的剧烈水热活性。这些结果将脊分割的模型相互矛盾，其分别预测段中心下方的增强和降低的熔体供应。我们的结果支持一种模型，其中地壳和地幔岩石系统之间的分段尺度歪斜控制中海脊的岩石和水热过程。 </ 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21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=Arnoux G. M.&option=202" target="_blank" rel="nofollow">Arnoux G. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Toomey D. R.&option=202" target="_blank" rel="nofollow">Toomey D. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hooft E. E. E.&option=202" target="_blank" rel="nofollow">Hooft E. E. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilcock W. S. D.&option=202" target="_blank" rel="nofollow">Wilcock W. S. D.;</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 Earth SciencesUniversity of OregonEugene OR USA;</p> <p>Department of Earth SciencesUniversity of OregonEugene OR USA;</p> <p>Department of Earth SciencesUniversity of OregonEugene OR USA;</p> <p>School of OceanographyUniversity 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=mid‐ocean ridges&option=203" rel="nofollow">mid‐ocean ridges;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Juan de Fuca Ridge&option=203" rel="nofollow">Juan de Fuca Ridge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic crust&option=203" rel="nofollow">oceanic crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydrothermal systems&option=203" rel="nofollow">hydrothermal systems;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seismic tomography&option=203" rel="nofollow">seismic tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=thermal structure&option=203" rel="nofollow">thermal structure;</a> </p> <div class="translation"> 机译：中海山脊;Juan de Fuca岭;海壳;水热系统;地震层析成像;热结构; </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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360521.html">Seismic Imaging and Physical Properties of the Endeavour Segment: Evidence that Skew Between Mantle and Crustal Magmatic Systems Governs Spreading Center Processes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arnoux G. 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