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Watching Dehydration: Seismic Indication for Transient Fluid Pathways in the Oceanic Mantle of the Subducting Nazca Slab

机译：观看脱水：粪便裸露植物隧道瞬态流体途径的地震迹象

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Abstract > Intermediate depth seismicity in subduction zones often occurs in the form of two slab‐parallel bands. We estimated the seismic <fi>P</fi> to <fi>S</fi> wave velocity ratio within the shallowest part of the lower seismicity zone (LSZ) in the mantle of the subducting slab of the Central Andean subduction system at 50‐km depth, 30?km below the Moho, using local earthquake data. We find an exceptionally high <fi>V</fi> <sub> <fi>P</fi> </sub> / <fi>V</fi> <sub> <fi>S</fi> </sub> value larger than ～2.0 that cannot be explained by a realistic solid lithology but requires the presence of fluid‐filled porosity. This implies that the incoming Nazca plate must be partially hydrated to this depth below the seafloor. We introduce a state‐of‐the‐art petrophysical model that takes into account the thermodynamic and poroelastic effects of dynamic metamorphic mineral dehydration at 1.8?GPa and consider anisotropic effects. The model shows that a high <fi>V</fi> <sub> <fi>P</fi> </sub> / <fi>V</fi> <sub> <fi>S</fi> </sub> value generally indicates that the medium is near the percolation threshold, that is, that porosity must be interconnected. This result is consistent with observations from outcrops of paleosubduction zones, laboratory experiments, and numerical simulations. It follows that the shallowest part of the LSZ of the Central Andes must reside at a temperature at which mineral dehydration reactions take place, here between 430 and 500?° C. For the first time, we can confirm that the observations of transient dehydrating fluid‐filled vein structures with a pore volume in the order of only 10 ?3 are reasonable for the LSZ and enough to allow for effective drainage. </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 =“GGGE21670-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> > 俯冲区域中的中间深度地震性经常以两个平行的带的形式发生。我们估计了地震 <fi> p </ fi> 到 <fi> s </ fi> 下部地震区（LSZ）中最浅部分内的波速比在中央和平俯冲系统的窗口板块的窗幔中，50公里深度，使用当地地震数据在MOHO以下30克。我们发现一个特别高 <fi> v </ fi> <sub> <fi> p </ fi> </ sub> / <fi> v </ fi> <sub> <fi> s </ fi> </ sub> 值大于〜2.0，无法通过现实的固体岩性解释，但需要存在流体填充的孔隙率。这意味着进入的NaZCA板必须部分地水合到海底下方的该深度。我们介绍了一种最先进的岩石物理模型，考虑到动态变质矿物脱水的热力学和多孔弹性效果在1.8？GPA，并考虑各向异性效应。该模型表明很高 <fi> v </ fi> <sub> <fi> p </ fi> </ sub> / <fi> v </ fi> <sub> <fi> s </ fi> </ sub> 值通常表明介质接近渗透阈值，即必须互连孔隙率。该结果与从古软化区，实验室实验和数值模拟的露头的观察结果一致。所以遵循中央和中央和中央的最浅部分必须位于矿物脱水反应发生的温度下，这里首次在430和500℃之间进行，我们可以确认瞬时脱水液的观察 - 仅为仅10的孔隙体积的静脉结构？3 </ sup> 对LSZ合理，足以允许有效的排水。 </ 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>2018年第9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=Bloch Wasja&option=202" target="_blank" rel="nofollow">Bloch Wasja;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=John Timm&option=202" target="_blank" rel="nofollow">John Timm;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kummerow J?rn&option=202" target="_blank" rel="nofollow">Kummerow J?rn;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Salazar Pablo&option=202" target="_blank" rel="nofollow">Salazar Pablo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krüger Oliver S.&option=202" target="_blank" rel="nofollow">Krüger Oliver S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shapiro Serge A.&option=202" target="_blank" rel="nofollow">Shapiro Serge 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>Freie Universit?t BerlinBerlin Germany;</p> <p>Freie Universit?t BerlinBerlin Germany;</p> <p>Freie Universit?t BerlinBerlin Germany;</p> <p>Universidad Católica del NorteAntofagasta Chile;</p> <p>Freie Universit?t BerlinBerlin Germany;</p> <p>Freie Universit?t BerlinBerlin Germany;</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;"> </p> </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/0704023360728.html">Watching Dehydration: Seismic Indication for Transient Fluid Pathways in the Oceanic Mantle of the Subducting Nazca Slab</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bloch Wasja&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bloch Wasja,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=John Timm&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">John Timm,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kummerow J?rn&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kummerow J?rn,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</span><span>,第9期</span> </span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：观看脱水：粪便裸露植物隧道瞬态流体途径的地震迹象</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704018512168.html">Seismic evidence for rotating mantle flow around subducting slab edge associated with oceanic microplate capture</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stephen G. 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