Miocene Glacial Dynamics Recorded by Variations in Magnetic Properties in the ANDRILL‐2A Drill Core

机译：通过Andrill-2a钻芯中磁性特性的变化记录的内肾冰川动力学

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Abstract >During the 2007 ANtarctic geological DRILLing (ANDRILL) campaign in the Ross Sea, Antarctica, the AND‐2A core was recovered through a stratigraphic succession spanning 1,138.54?m of Neogene sedimentary rocks that include an expanded early to middle Miocene sequence. The study reported here focuses on the magnetic properties of the interval from 778.63?m below sea floor (mbsf) to 1,138.54?mbsf, which comprises a time interval spanning 1.5?Myr, from ~18.7 to ~20.2?Ma. We recognize three main pulses of increased input of magnetic materials to the drill site between 778.34–903.06, 950.55–995.78, and 1,040–1,103.96?mbsf. Trends in the magnetic mineral concentration dependent parameters mirror changes in the proportion of sediments derived from McMurdo Volcanic Group rocks. We suggest that these pulses in magnetic mineral concentration reflect changes in sediment transport processes associated with changing glacial conditions at the drill site that included (1) subglacial and grounding zone proximal settings, (2) hemipelagic and neritic conditions with abundant sediment‐rich icebergs, and (3) grounding zone‐distal environment that was covered by land‐fast multiyear sea ice or a fringing ice shelf. The magnetic minerals record preserved in the AND‐2A core supports other data that indicate a highly dynamic and variable coastal environment during the early Miocene, where glaciers retreated inland under warm climatic conditions and advanced beyond the drill site across the continental shelf when cold climate prevailed. </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> >在2007年南极地质钻井（andrill）竞选中，南极洲，南极洲，和-2A核心通过跨越1,138.54？m的地层继承来恢复Neogene沉积岩，其包括早期中均匀序列的扩展。本研究报告的研究侧重于海底（MBSF）下方778.63Ω米的间隔磁性（MBSF）至1,138.54Ω·MBSF，其包括跨越1.5的时间间隔，从〜18.7到〜20.2？mA。我们认识到磁性材料的增加的三个主要脉冲到钻头部位，在778.34-903.06,950.55-995.78和1,040-1,103.96？MBSF之间。磁性矿物浓度依赖性参数镜像镜比例的沉积物比例从MCMURDO火山群岩石的比例变化。我们建议磁矿物质浓度中的这些脉冲反映了与在钻头部位的冰川条件改变冰川条件相关的沉积物传输过程的变化，其中包括（1）底裂和接地区近端设置，（2）Hemiphic和Neritic条件具有丰富的沉积物的冰山，（3）接地区域 - 远端环境被陆地快速的多年海冰或流苏冰架覆盖。保留在AND-2A核心中的磁性矿物质记录支持其他数据，这些数据在早期的中生期间表明高度动态和可变的沿海环境，冰川在温暖气候条件下撤退内陆，当冷酷的气候普遍存在。</ 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>2019年第3期</span><b style="margin: 0 2px;">|</b><span>共16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=Jovane Luigi&option=202" target="_blank" rel="nofollow">Jovane Luigi;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Florindo Fabio&option=202" target="_blank" rel="nofollow">Florindo Fabio;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Acton Gary&option=202" target="_blank" rel="nofollow">Acton Gary;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ohneiser Christian&option=202" target="_blank" rel="nofollow">Ohneiser Christian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sagnotti Leonardo&option=202" target="_blank" rel="nofollow">Sagnotti Leonardo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Strada Eleonora&option=202" target="_blank" rel="nofollow">Strada Eleonora;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Verosub Kenneth L.&option=202" target="_blank" rel="nofollow">Verosub Kenneth L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wilson Gary S.&option=202" target="_blank" rel="nofollow">Wilson Gary S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Iacoviello Francesco&option=202" target="_blank" rel="nofollow">Iacoviello Francesco;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Levy Richard H.&option=202" target="_blank" rel="nofollow">Levy Richard H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Passchier Sandra&option=202" target="_blank" rel="nofollow">Passchier Sandra;</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>Instituto Oceanográfico da Universidade de S?o PauloS?o Paulo SP Brazil;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>International Ocean Discovery Program Texas A&</p> <p>M UniversityCollege StationTX USA;</p> <p>Department of GeologyUniversity of OtagoDunedin New Zealand;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>Department of Earth and Planetary SciencesUniversity of CaliforniaDavis CA USA;</p> <p>Department of GeologyUniversity of OtagoDunedin New Zealand;</p> <p>Instituto Oceanográfico da Universidade de S?o PauloS?o Paulo SP Brazil;</p> <p>Department of PaleontologyGNS ScienceLower Hutt New Zealand;</p> <p>Department of Earth and Environmental SciencesMontclair State UniversityMontclair NJ 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=ANDRILL&option=203" rel="nofollow">ANDRILL;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ross Sea&option=203" rel="nofollow">Ross Sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Southern McMurdo Sound&option=203" rel="nofollow">Southern McMurdo Sound;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Antarctica&option=203" rel="nofollow">Antarctica;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=early Miocene&option=203" rel="nofollow">early Miocene;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magnetic properties&option=203" rel="nofollow">magnetic properties;</a> </p> <div class="translation"> 机译：andrill;罗斯大海;南麦克马多的声音;南极洲;早期内科;磁性; 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initial;text-overflow: initial;overflow: initial;"> <span>机译：确定通过对地下材料的芯体进行钻孔而获得的芯的取向的方法，所述方法包括确定钻孔的振动处于或低于指定的振动水平，相关数据记录You，将本体与地基的核心，并从数据记录中获取Nucleus的设备方向。 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130491383215.html">Circuit arrangement for review of the magnetic properties of magnetic cores according to the difference method and for the sorting of the cores</a> <b>[P]</b> . <span> 外国专利：  DE1089475B </span> <span> . 1960-09-22</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：用于根据差值方法检查磁芯的磁特性并进行磁芯分类的电路装置 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 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