Pockmarks in the Witch Ground Basin, Central North Sea

机译：巫术盆地，中央北海的巫术

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Abstract > Marine sediments host large amounts of methane (CH4), which is a potent greenhouse gas. Quantitative estimates for methane release from marine sediments are scarce, and a poorly constrained temporal variability leads to large uncertainties in methane emission scenarios. Here, we use 2‐D and 3‐D seismic reflection, multibeam bathymetric, geochemical, and sedimentological data to (I) map and describe pockmarks in the Witch Ground Basin (central North Sea), (II) characterize associated sedimentological and fluid migration structures, and (III) analyze the related methane release. More than 1,500 pockmarks of two distinct morphological classes spread over an area of 225?km 2 . The two classes form independently from another and are corresponding to at least two different sources of fluids. Class 1 pockmarks are large in size (6?m deep, 250?m long, and 75?m wide), show active venting, and are located above vertical fluid conduits that hydraulically connect the seafloor with deep methane sources. Class 2 pockmarks, which comprise 99.5% of all pockmarks, are smaller (0.9–3.1?m deep, 26–140?m long, and 14–57?m wide) and are limited to the soft, fine‐grained sediments of the Witch Ground Formation and possibly sourced by compaction‐related dewatering. Buried pockmarks within the Witch Ground Formation document distinct phases of pockmark formation, likely triggered by external forces related to environmental changes after deglaciation. Thus, greenhouse gas emissions from pockmark fields cannot be based on pockmark numbers and present‐day fluxes but require an analysis of the pockmark forming processes through geological time. </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> > 海洋沉积物宿主大量的甲烷（CH4），这是一个有效的温室气体。海洋沉积物的甲烷释放的定量估计是稀缺的，并且受到严重的时间变异性导致甲烷发射场景中的大不确定性。在这里，我们使用2-D和3-D地震反射，多沟碱基，地球化学和沉积学数据到（i）地图并描述巫术盆地（中央北海）的麻木，（ii）的特征在于相关的沉积学和液体迁移结构和（iii）分析相关的甲烷释放。超过1,500多个不同的形态学课程蔓延到225 km 2 </ sup> 。两种类别从另一个阶层形成，并且对应于至少两个不同的流体来源。 1级尺寸大小（＆ 6？m深，＆长度为250μm，长75米宽），显示出主动通风，并且位于垂直流体管道上方，用深甲烷液压连接海底。来源。 2级Pockmarks，其中包括99.5％的所有麻木，较小（深度为0.9-3.1米，长26-140米长，宽度为14-57？M宽），并限于柔软，细粒度的沉积物巫术地面形成，可能通过压实相关的脱水来源。埋藏在巫术地面形成文件中的埋藏阶段的Pockmark地层阶段，可能被与环境变化相关的外部力量引发。因此，来自Pockmark Fields的温室气体排放不能基于Pockmark数和当前的通量，而是需要通过地质时间分析Pockmark形成过程。 </ 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>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共22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=B?ttner Christoph&option=202" target="_blank" rel="nofollow">B?ttner Christoph;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Berndt Christian&option=202" target="_blank" rel="nofollow">Berndt Christian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Reinardy Benedict T.I.&option=202" target="_blank" rel="nofollow">Reinardy Benedict T.I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Geersen Jacob&option=202" target="_blank" rel="nofollow">Geersen Jacob;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Karstens Jens&option=202" target="_blank" rel="nofollow">Karstens Jens;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bull Jonathan M.&option=202" target="_blank" rel="nofollow">Bull Jonathan M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Callow Ben J.&option=202" target="_blank" rel="nofollow">Callow Ben J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lichtschlag Anna&option=202" target="_blank" rel="nofollow">Lichtschlag Anna;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schmidt Mark&option=202" target="_blank" rel="nofollow">Schmidt Mark;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Elger Judith&option=202" target="_blank" rel="nofollow">Elger Judith;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schramm Bettina&option=202" target="_blank" rel="nofollow">Schramm Bettina;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haeckel Matthias&option=202" target="_blank" rel="nofollow">Haeckel Matthias;</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>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>Stockholm University and Bolin Centre for Climate ResearchStockholm Sweden;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>Ocean and Earth ScienceUniversity of Southampton National Oceanography CentreSouthampton UK;</p> <p>Ocean and Earth ScienceUniversity of Southampton National Oceanography CentreSouthampton UK;</p> <p>National Oceanography CentreUniversity of Southampton Waterfront CampusSouthampton UK;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</p> <p>GEOMAR Helmholtz Centre for Ocean Research KielKiel Germany;</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=hydrocarbon&option=203" rel="nofollow">hydrocarbon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=seepage&option=203" rel="nofollow">seepage;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=fluid flow&option=203" rel="nofollow">fluid flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=glaciology&option=203" rel="nofollow">glaciology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=quaternary geology&option=203" rel="nofollow">quaternary geology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=sedimentology&option=203" rel="nofollow">sedimentology;</a> </p> <div class="translation"> 机译：碳氢化合物;渗流;流体流动;冰川学;第四纪地质学;沉积学; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 03:08:00</span> </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/0704023360798.html">Pockmarks in the Witch Ground Basin, Central North Sea</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=B?ttner Christoph&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">B?ttner Christoph,</a> <a 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