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首页> 外文期刊>Geophysical Research Letters >Depth‐Dependent Geometry of the Liqui?e‐Ofqui Fault Zone and Its Relation to Paths of Slab‐Derived Fluids
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Depth‐Dependent Geometry of the Liqui?e‐Ofqui Fault Zone and Its Relation to Paths of Slab‐Derived Fluids

机译:Liqui的深度依赖性几何形状及其与平板衍生的流体路径的关系

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摘要

Abstract >Using a nonhomogeneous elastic model for the south Chile subduction zone, we calculate the depth‐dependent geometry of the Liqui?e‐Ofqui Fault Zone (LOFZ), considering that faults develop where shear stress is maximum. Shear stress develops due to the oblique subduction process, depending on shear modulus which varies as a function of the amount of fluids within the overriding plate. Regions with different values of shear modulus are obtained by the geometries of isotherms calculated from a thermal model. Based on the principle that fluids move from higher to lower pressure regions, we calculate paths of fluids from the subducting slab toward the free surface. In the vicinity of the volcanic arc, the obtained fluid paths agree with the geometry of the LOFZ, suggesting that margin‐parallel strike‐slip faults could serve as pathways for fluids through the overriding plate in oblique subduction zones. </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:ID =“Grl56500-Abs-Abs-0001”XML:Lang =“en”> <标题类型=“main”>抽象</ title> >使用南方的非均匀弹性模型智利俯冲区,我们计算Liqui的深度依赖性几何形状(Lofz),考虑到剪切应力最大的故障发生。由于倾斜的俯冲过程,剪切应力发生,这取决于剪切模量,其变化,其变化,其变化,其变化,其变化为近侧的流体量的函数。具有不同剪切模量值的区域通过从热模型计算的等温物质的几何来获得。基于流体从较高到较低压力区域移动的原理,我们计算从底板板朝向自由表面的流体的路径。在Volcanic弧附近,所获得的流体路径与Lofz的几何形状一致,表明边缘平行的击球故障可以用作通过倾斜俯冲区域的覆盖板的流体的途径。</ 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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2017年第21期</span><b style="margin: 0 2px;">|</b><span>共5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=Catalán N.&option=202" target="_blank" rel="nofollow">Catalán N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bataille K.&option=202" target="_blank" rel="nofollow">Bataille K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Araya R.&option=202" target="_blank" rel="nofollow">Araya R.;</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>Departamento de Ciencias de la Tierra Facultad de Ciencias QuímicasUniversidad de ConcepciónConcepción Chile;</p> <p>Departamento de Ciencias de la Tierra Facultad de Ciencias QuímicasUniversidad de ConcepciónConcepción Chile;</p> <p>Departamento de Ingeniería Matemática &</p> <p>CI2MAUniversidad de ConcepciónConcepción Chile;</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=oblique subduction&option=203" rel="nofollow">oblique subduction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=margin‐parallel strike‐slip faults&option=203" rel="nofollow">margin‐parallel strike‐slip faults;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid migration&option=203" rel="nofollow">fluid migration;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=southern Chile&option=203" rel="nofollow">southern Chile;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liqui?e‐Ofqui Fault Zone&option=203" rel="nofollow">Liqui?e‐Ofqui Fault Zone;</a> </p> <div class="translation"> 机译:倾斜俯冲;边缘平行的滑行故障;流体迁移;智利南部;Lifi?E-Ofqui断层区域; </div> </li> </ul> </div> </div> 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