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Structure, Seismicity, and Accretionary Processes at the Hot Spot‐Influenced Axial Seamount on the Juan de Fuca Ridge

机译：在Juan de Fuca Ridge的热点影响轴山轴上的结构，地震性和增生过程

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Abstract > Axial Seamount is the most volcanically active site of the northeast Pacific, and it has been monitored with a growing set of observations and sensors during the last two decades. Accurate imaging of the internal structure of volcanic systems is critical to better understand magma storage processes and to quantify mass and energy transport mechanisms in the crust. To improve the three‐dimensional velocity structure of Axial Seamount, we combined 469,891 new traveltime arrivals, from 12 downward extrapolated seismic profiles, with 3,962 existing ocean‐bottom‐seismometers traveltime arrivals, into a joint tomographic inversion. Our approach reveals two elongated magma reservoirs, with melt fraction up to 65%, representing an unusually large volume of melt (26–60?km 3 ), which is likely the result of enhanced magma supply from the juxtaposition of the Cobb hot spot plume (0.26–0.53?m 3 /s) and the Axial spreading segment (0.79–1.06?m 3 /s). The tomographic model also resolves a subsided caldera floor that provides an effective trap for ponding lava flows, via a “trapdoor” mechanism. Our model also shows that Axial's extrusive section is thinnest beneath the elevated volcano, where anomalously thick (11?km) oceanic crust is present. We therefore suggest that focused and enhanced melt supply predominantly thickens the crust beneath Axial Seamount through diking accretion and gabbro crystallization. Lastly, we demonstrate that our three‐dimensional velocity model provides a more realistic starting point for relocating the local seismicity, better resolving a network of conjugate outward and inward dipping faults beneath the caldera walls.?2018. The Authors. </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”> <Title Type =“main”>抽象</ title> >轴向海米是东北太平洋最储蓄的场地，它已被监控在过去二十年中，一套不断增长的观测和传感器。对火山系统的内部结构的精确成像对于更好地了解岩浆存储过程并在地壳中量化质量和能量传输机制至关重要。为了提高轴向海山的三维速度结构，我们组合了469,891个新的旅行时间抵达，从12个向下推断的地震曲线，3,962个海底地震仪旅行时间到达，进入一个关节断层倒置。我们的方法揭示了两个细长的岩浆储层，熔体分数高达65％，代表了异常大量的熔体（26-60 km 3 </ sup>），这可能是增强岩浆供应的结果COBB热点羽流的并置（0.26-0.53？m 3 </ sup> / s）和轴向扩展段（0.79-1.06Ωm 3 </ sup> s）。断层图模型还可以通过“陷阱”机制来解决一个消耗的CALDERA地板，该地板提供了有效的疏水阀流动流动的陷阱。我们的模型还表明，轴向的喷射部分在升高的火山下方最薄，在那里存在异常厚（11 km）海洋地壳。因此，我们表明，聚焦和增强的熔体供应主要通过沿着散热器和加法结晶来使轴向山脉下方的外壳增厚。最后，我们证明我们的三维速度模型提供了更现实的起点，用于重新定位当地地震性，更好地解析在卡尔德拉墙壁下方的外向和向内倾倒故障的缀合物网络。作者。 </ p> </ abstract> </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6期</span><b style="margin: 0 2px;">|</b><span>共29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=Arnulf A. F.&option=202" target="_blank" rel="nofollow">Arnulf A. F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Harding A. J.&option=202" target="_blank" rel="nofollow">Harding A. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kent G. M.&option=202" target="_blank" rel="nofollow">Kent G. M.;</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>Institute for Geophysics Jackson School of GeosciencesUniversity of Texas at AustinAustin TX USA;</p> <p>Cecil H. and Ida M. Green Institute of Geophysics and Planetary Physics Scripps Institution of OceanographyUniversity of California San DiegoLa Jolla CA USA;</p> <p>Nevada Seismological LaboratoryUniversity of Nevada RenoReno NV 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=traveltime tomography&option=203" rel="nofollow">traveltime tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Axial Seamount&option=203" rel="nofollow">Axial Seamount;</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=hot spot&option=203" rel="nofollow">hot spot;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magmatic system&option=203" rel="nofollow">magmatic system;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcano&option=203" rel="nofollow">volcano;</a> </p> <div class="translation"> 机译：旅行时间断层扫描;轴向海山;Juan de Fuca岭;热点;岩浆系统;火山; </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/0704025591245.html">Structure, Seismicity, and Accretionary Processes at the Hot Spot‐Influenced Axial Seamount on the Juan de Fuca Ridge</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Arnulf A. 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