Anomalous Pacific‐Antarctic Ridge Volcanism Precedes Glacial Termination 2

机译：异常的太平洋 - 南极脊火山前冰川终止2

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Abstract >We present results from a well‐dated sediment core on the Pacific‐Antarctic Ridge (PAR) that document a ～15 cm thick layer of basaltic ash shards that precedes the penultimate deglaciation (Termination 2). The glasses have MORB composition consistent with an axial source and their morphologies are typical of pyroclastic deposits created by submarine volcanism. The ash layer was deposited ～7 km from the PAR axis, a distance that implies buoyant plumes lofted debris high into the water column with subsequent fallout to the core location. We infer plume rise height using grain settling velocities, the water depth at the core site, and deep ocean current speeds from ARGO floats. Rise heights of 1.5 km or less require unrealistically large current speeds to transport grains to the core site. Instead, the data are consistent with a plume rise height of at least 2 km, implying that T2 was an interval of anomalous volcanism along this segment of the PAR. The timing and duration of the ash deposit is consistent with glacial‐interglacial modulation of ridge magmatism. Volcaniclastic records from additional locations will be necessary to assess whether the PAR record is a rare find or it is representative of mid‐ocean ridge volcanism during glacial terminations. </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> >我们在太平洋 - 南极脊上的富日期沉积物核心（PAR）上的结果提出，记录了倒倒倒倒在倒数第二次玄武岩碎片层（终止2）之前的玄武岩灰分碎片。眼镜的Morb组合物与轴向源一致，它们的形态是由潜艇火山中产生的典型的吡芯弹性沉积物。灰层沉积距离轴~7公里，距离浮气羽状的碎片高到水柱中，随后的辐射到核心位置。我们使用谷物沉降速度，核心位点的水深以及Argo浮子的深远电流速度推断出羽毛升高。上升高度为1.5公里或更少需要不切实际的电流速度将谷物运输到核心位置。相反，数据与至少2公里的流量上升高度一致，暗示T2是沿着该阵容的这种段的异常火山的间隔。灰度沉积的时序和持续时间与脊岩浆的冰川层间调制一致。来自其他地点的火山可记录是必要的，以评估PAR记录是否是罕见的发现，或者在冰川终止期间代表中海岭火山。</ 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8期</span><b style="margin: 0 2px;">|</b><span>共14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=Lund David C.&option=202" target="_blank" rel="nofollow">Lund David C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Seeley Emily I.&option=202" target="_blank" rel="nofollow">Seeley Emily I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Asimow Paul D.&option=202" target="_blank" rel="nofollow">Asimow Paul D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lewis Madeline J.&option=202" target="_blank" rel="nofollow">Lewis Madeline J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McCart Sarah E.&option=202" target="_blank" rel="nofollow">McCart Sarah E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mudahy Annalisa A.&option=202" target="_blank" rel="nofollow">Mudahy Annalisa 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>Department of Marine SciencesUniversity of ConnecticutCT USA;</p> <p>Department of Marine SciencesUniversity of ConnecticutCT USA;</p> <p>Division of Geological and Planetary SciencesCalifornia Institute of TechnologyCA USA;</p> <p>Division of Geological and Planetary SciencesCalifornia Institute of TechnologyCA USA;</p> <p>Department of Marine SciencesUniversity of ConnecticutCT USA;</p> <p>Department of Marine SciencesUniversity of ConnecticutCT 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=volcanism&option=203" rel="nofollow">volcanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glacial&option=203" rel="nofollow">glacial;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=interglacial&option=203" rel="nofollow">interglacial;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pacific Antarctic Ridge&option=203" rel="nofollow">Pacific Antarctic Ridge;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Termination 2&option=203" rel="nofollow">Termination 2;</a> </p> <div class="translation"> 机译：火山主义;冰川;中间夹;太平洋南极脊;终止2; 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