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The Final Stages of Slip and Volcanism on an Oceanic Detachment Fault at 13°48′N, Mid‐Atlantic Ridge

机译：13°48'N，中大西洋山脊的海洋分离错误的滑倒和火山的最终阶段

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Abstract > While processes associated with initiation and maintenance of oceanic detachment faults are becoming better constrained, much less is known about the tectonic and magmatic conditions that lead to fault abandonment. Here we present results from near‐bottom investigations using the submersible Alvin and autonomous underwater vehicle Sentry at a recently extinct detachment fault near 13°48′N, Mid‐Atlantic Ridge, that allow documentation of the final stages of fault activity and magmatism. Seafloor imagery, sampling, and near‐bottom magnetic data show that the detachment footwall is intersected by an ~850 m‐wide volcanic outcrop including pillow lavas. Saturation pressures in these vesicular basalts, based on dissolved H <sub>2</sub> O and CO <sub>2</sub> , are less than their collection pressures, which could be explained by eruption at a shallower level than their present depth. Sub‐bottom profiles reveal that sediment thickness, a loose proxy for seafloor age, is ~2?m greater on top of the volcanic terrain than on the footwall adjacent to the hanging‐wall cutoff. This difference could be explained by current‐driven erosion in the axial valley or by continued slip after volcanic emplacement, on either a newly formed or pre‐existing fault. Since current speeds near the footwall are unlikely to be sufficient to cause significant erosion, we favor the hypothesis that detachment slip continued after the episode of magmatism, consistent with growing evidence that oceanic detachments can continue to slip despite hosting magmatic intrusions. </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> > 虽然与海洋脱离故障的启动和维护相关的过程变得更好的约束，但关于导致故障遗弃的构造和岩石条件，尚不少。在这里，我们使用潜水的近底调查显示结果 alvin </ i> 和自动水下车辆哨兵</ i> 在最近灭绝的拆卸断层近13°48'n，中大西洋山脊附近，允许文件的最终阶段的故障活动和岩浆。海底图像，取样和近底磁数据表明，脱离脚蹼与〜850米宽的火山露头相交，包括枕头熔岩。基于溶解的H的这些囊泡基础上的饱和压力 <sub> 2 </ sub> o和co. <sub> 2 </ sub> ，少于它们的收集压力，这可以通过比其目前深度的浅水平爆发来解释。次底型材揭示了沉积物厚度，海底时代的松散代理，在火山地顶上大约2？米，而不是悬挂式悬挂式截止的脚踏板上。这种差异可以通过轴谷的电流驱动的侵蚀来解释，或者在火山液位后继续滑动，在新形成或预先存在的故障上。由于脚踏壁附近的电流速度不太可能造成显着的侵蚀，因此有利于在岩浆广告发作后继续脱离拆卸的假设，符合日益增长的证据，尽管托管岩浆入侵，但是海运脱落可以继续滑动。 </ 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13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=Parnell‐Turner R. E.&option=202" target="_blank" rel="nofollow">Parnell‐Turner R. E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mittelstaedt E.&option=202" target="_blank" rel="nofollow">Mittelstaedt E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kurz M. D.&option=202" target="_blank" rel="nofollow">Kurz M. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jones M. R.&option=202" target="_blank" rel="nofollow">Jones M. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Soule S. A.&option=202" target="_blank" rel="nofollow">Soule S. A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klein F.&option=202" target="_blank" rel="nofollow">Klein F.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wanless V. D.&option=202" target="_blank" rel="nofollow">Wanless V. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fornari D. J.&option=202" target="_blank" rel="nofollow">Fornari D. J.;</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>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Department of Geological SciencesUniversity of IdahoMoscow ID USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Massachusetts Institute of Technology/Woods Hole Oceanographic Institution Joint Program in OceanographyWoods Hole MA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA USA;</p> <p>Department of GeosciencesBoise State UniversityBoise ID USA;</p> <p>Woods Hole Oceanographic InstitutionWoods Hole MA 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 ridge&option=203" rel="nofollow">mid‐ocean ridge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=oceanic detachment fault&option=203" rel="nofollow">oceanic detachment fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=near‐bottom geophysics&option=203" rel="nofollow">near‐bottom geophysics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volatile geochemistry&option=203" rel="nofollow">volatile geochemistry;</a> </p> <div class="translation"> 机译：海洋山脊;海洋脱离故障;近底地球物理;挥发性地球化学; </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/0704023360486.html">The Final Stages of Slip and Volcanism on an Oceanic Detachment Fault at 13°48′N, Mid‐Atlantic Ridge</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Parnell‐Turner R. 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