Neogene palaeoceanographic changes recorded in a carbonate contourite drift (Santaren Channel, Bahamas)

机译：Neogene古文献变化记录在碳酸盐盐漂移（Santaren频道，巴哈马）中

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Abstract >The Santaren Drift between the Great Bahama Bank and Cay Sal Bank (Bahamas) is closely linked to the development of the Gulf Stream and its shape and geometry record the local to global oceanographic, climatic and tectonic events since the Miocene. High‐resolution multichannel seismic data from the Santaren Channel allow detailed insight into the growth phases of the contourite drift, and by using the stratigraphic information from Ocean Drilling Program Site 1006 to infer its sedimentation rates. The results bring new understanding to this region and to interpretation of carbonate drifts. The data document that the signatures of a bottom current flow in the Santaren Channel initiated about 12·3?Ma, as indicated by the first occurrence of sheeted drifts and moat development at the northern part of the Santaren Channel. Narrowing and steepening of moat flanks as well as the pronounced upslope migration of the moat reflects a sustained current acceleration of the bottom currents until 5·5?Ma, associated with a transformation into mounded elongated drifts. Between 5·5?Ma and 3·1?Ma, bottom current intensity reached its maximum probably caused by the final closure of the Central American Seaway. The last 3·1?Myr were characterized by a marked increase in volume through flow reaching a maximum during the past 900?kyr. Drift growth was driven by the combined sources of export from the shallow‐water carbonate factory and by pelagic rain. The Middle Miocene channel‐related sheeted drift of the inner Santaren Channel is characterized by low accumulation rates, but a rapid increase of accumulation rates occurred during the Early Pliocene. The contourite drift buildup was disturbed by minor erosional phases with narrow moats in the Late Pliocene due to increasing bottom‐current velocities forced by strengthened Atlantic Ocean ventilation. The Early Ple </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 =“sed12573-abs-0001”xml：lang =“en”> <title type =“main”>抽象</ title> >伟大的Bahama银行之间的Santaren漂移和Cay Sal Bank（巴哈马）与海湾流的发展和几何形状的发展紧密相关，以自新世纪以来将当地的全球海洋，气候和构造事件记录。来自Santaren频道的高分辨率多通道地震数据允许详细介绍Contulite漂移的生长阶段，并通过使用来自海洋钻井计划网站1006的地层信息来推断其沉降率。结果为该地区带来了新的理解并解释了碳酸盐漂移。数据文档，即Santaren通道中的底部电流流动的签名引发了大约12·3？mA，如Santaren通道北部的第一次出现的片状漂移和护城河发育所示。护城河侧翼的狭窄和陡峭的护城河迁移的沉降反映了底部电流的持续电流加速度，直到5·5？mA，与转变成浑浊的细长漂移。在5·5？ma和3·1？ma之间，底部电流强度达到最大可能是由中美洲海滨的最终关闭引起的。最后3·1？MYR的特征在于，通过流量达到最大值在过去的900中达到最大值，其特征在于，在过去的900中达到最大值。漂移增长是由浅水碳酸盐厂和川芎的综合转型来源驱动。内部桑塔伦通道的中间内肾通道相关的片状漂移的特征在于累积率低，但在早期的全烯期间发生的积累速率的快速增加。由于加强大西洋通风的底部电流速度增加，在晚期腐烂的较窄的MoATS中，在狭窄的MoAT中，漂移阶段受到狭窄的侵蚀阶段的干扰。早期的地方 </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-28547/'>《Sedimentology: Journal of the International Association of Sedimentologists》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共25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=Paulat Marco&option=202" target="_blank" rel="nofollow">Paulat Marco;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lüdmann Thomas&option=202" target="_blank" rel="nofollow">Lüdmann Thomas;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Betzler Christian&option=202" target="_blank" rel="nofollow">Betzler Christian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Eberli Gregor P.&option=202" target="_blank" rel="nofollow">Eberli Gregor P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Frank Tracy&option=202" target="_blank" rel="nofollow">Frank Tracy;</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>Institut für GeologieUniversit?t HamburgBundesstrasse 55 Hamburg 20146 Germany;</p> <p>Institut für GeologieUniversit?t HamburgBundesstrasse 55 Hamburg 20146 Germany;</p> <p>Institut für GeologieUniversit?t HamburgBundesstrasse 55 Hamburg 20146 Germany;</p> <p>CSL ‐ Center for Carbonate ResearchUniversity of MiamiMiami FL 33149 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/165.html" title="地质学">地质学;</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=Atlantic Ocean&option=203" rel="nofollow">Atlantic Ocean;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bahamas&option=203" rel="nofollow">Bahamas;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bottom current&option=203" rel="nofollow">bottom current;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=carbonate platform&option=203" rel="nofollow">carbonate platform;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=contourite drift&option=203" rel="nofollow">contourite drift;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=moat geometry&option=203" rel="nofollow">moat geometry;</a> </p> <div class="translation"> 机译：大西洋;巴哈马;底部电流;碳酸盐平台;轮廓石漂移;护城河几何; 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href="/patent-detail/06120110401217.html">用于高温度变化的无漂移HREM的MEMS装置中的多重加热器</a> <b>[P]</b> . <span> 中国专利： CN107924800A </span> <span> . 2018-04-17</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120102660026.html">通过碳酸盐和/或碳酸氢盐无机物的共同产生从废弃流中除去二氧化碳</a> <b>[P]</b> . <span> 中国专利： CN104069726A </span> <span> . 2014-10-01</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130479573217.html">DC drift eliminator for group of data channels - successively receives channel output and drift level and subtracts</a> <b>[P]</b> . <span> 外国专利：  FR2282759B1 </span> <span> . 1979-05-18</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：用于数据通道组的直流漂移消除器-连续接收通道输出和漂移电平并减去 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130482699960.html">DC drift eliminator for group of data channels - successively receives channel output and drift level and subtracts</a> <b>[P]</b> . <span> 外国专利：  FR2282759A1 </span> <span> . 1976-03-19</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：用于数据通道组的直流漂移消除器-连续接收通道输出和漂移电平并减去 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130441428142.html">Semiconducting arrangement with p- and n-channel transistors has transistors with drift paths with at least one region of opposite type to channel types and complementary symmetry in drift paths</a> <b>[P]</b> . <span> 外国专利：  DE10301496A1 </span> <span> . 2004-08-05</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：具有p沟道和n沟道晶体管的半导体装置具有漂移路径至少具有与沟道类型相反的区域并且漂移路径中互补对称的区域的漂移路径的晶体管。 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