On the Timing and Nature of the Multiple Phases of Slope Instability on Eastern Rockall Bank, Northeast Atlantic

Georgiopoulou A.; Krastel S.; Finch N.; Zehn K.; McCarron S.; Huvenne V. A. I.; Haughton P. D. W.; Shannon P. M.

摘要

Abstract > One of the most challenging tasks when studying large submarine landslides is determining whether the landslide was initiated as a single large event, a chain of events closely spaced in time or multiple events separated by long periods of time as all have implications in risk assessments. In this study we combine new multichannel seismic profiles and new sediment cores with bathymetric data to test whether the Rockall Bank Slide Complex, offshore western Ireland, is the composite of multiple slope collapse events and, if so, to differentiate them. We conclude that there have been at least three voluminous episodes of slope collapse separated by long periods of slope stability, a fourth, less voluminous event, and possibly a fifth more localized event. The oldest event, Slide A (200?km 3 ), is estimated to be several hundred thousand years old. The second event, Slide B (125?km 3 ), took place at the same location as slide A, reactivating the same scar, nearly 200?ka ago, possibly through retrogression of the scarp. Slide C (400?km 3 ) took place 22?ka ago and occurred further north from the other slides. Slide D was a much smaller event that happened 10?ka ago, while the most recent event, albeit very small scale, took place within the last 1,000?years. This study highlights the need to thoroughly investigate large slide complexes to evaluate event sequencing, as seismic studies may hide multiple small‐scale events. This work also reveals that the same slide scarps can be reactivated and generate slides with different flow behaviors. </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> > 学习大型潜艇滑坡时最具挑战性的任务之一是确定滑坡是否被发起为单一的大型事件，一系列事件在时间间隔或多个时间间隔的事件，因为所有人都有在风险评估中的影响。在这项研究中，我们将新的多通道地震曲线和新沉积物核心与碱基数据相结合，以测试摇滚银行幻灯片复杂，海上西尔兰，是多个斜坡塌陷事件的复合，如果是，则可以区分它们。我们得出结论，在长期的坡度稳定性，第四个，较少的大量事件中，至少有三个坡度坍塌发作，并且可能是第五个局部事件。最古老的事件，幻灯片A（200？Km 3 </ sup> ），估计数十万岁。第二次事件，幻灯片B（125 km 3 </ sup> ），在与幻灯片的幻灯片相同的位置发生在同一位置，再激活相同的疤痕，近200？ka前，可能是通过围巾的倒退。幻灯片C（400 km 3 </ sup> ）举行了22岁？ka前，从另一个幻灯片开始进一步北方。 Slide D是一个更小的事件发生了10？ka前，而最近的活动虽然非常小的比例，但在最后1000年内发生了。本研究突出了彻底调查大型幻灯片复合物来评估事件测序的需要，因为地震研究可能隐藏多个小规模事件。这项工作还揭示了可以重新激活相同的滑动轴，并产生具有不同流动行为的载玻片。 </ 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2期</span><b style="margin: 0 2px;">|</b><span>共20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=Georgiopoulou A.&option=202" target="_blank" rel="nofollow">Georgiopoulou A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krastel S.&option=202" target="_blank" rel="nofollow">Krastel S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Finch N.&option=202" target="_blank" rel="nofollow">Finch N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zehn K.&option=202" target="_blank" rel="nofollow">Zehn K.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=McCarron S.&option=202" target="_blank" rel="nofollow">McCarron S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huvenne V. A. I.&option=202" target="_blank" rel="nofollow">Huvenne V. A. I.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Haughton P. D. W.&option=202" target="_blank" rel="nofollow">Haughton P. D. W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shannon P. M.&option=202" target="_blank" rel="nofollow">Shannon P. M.;</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>UCD School of Earth SciencesUniversity College DublinDublin Ireland;</p> <p>Institute of GeosciencesChristian‐Albrechts‐Universit?t zu KielKiel Germany;</p> <p>UCD School of Earth SciencesUniversity College DublinDublin Ireland;</p> <p>Institute of GeosciencesChristian‐Albrechts‐Universit?t zu KielKiel Germany;</p> <p>Department of GeographyMaynooth UniversityMaynooth Ireland;</p> <p>National Oceanography CentreSouthampton University of Southampton Waterfront CampusSouthampton UK;</p> <p>UCD School of Earth SciencesUniversity College DublinDublin Ireland;</p> <p>UCD School of Earth SciencesUniversity College DublinDublin Ireland;</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=Rockall Bank Slide Complex&option=203" rel="nofollow">Rockall Bank Slide Complex;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=debrite&option=203" rel="nofollow">debrite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=multiphase slope collapse&option=203" rel="nofollow">multiphase slope collapse;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=British Irish Ice Sheet&option=203" rel="nofollow">British Irish Ice Sheet;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=bottom currents&option=203" rel="nofollow">bottom currents;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=flow transformation&option=203" rel="nofollow">flow transformation;</a> </p> <div class="translation"> 机译：Rockall Bank Slide Complex;Debrite;多相坡塌陷;英国爱尔兰冰盖;底部电流;流动转换; </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/0704023360761.html">On the Timing and Nature of the Multiple Phases of Slope Instability on Eastern Rockall Bank, Northeast Atlantic</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Georgiopoulou A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Georgiopoulou A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Krastel S.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Krastel S.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Finch N.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Finch N.,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2019</span><span>,第2期</span> </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：论东北大西洋东部岩石银行坡稳定性多阶段的时序与性质</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/070406328563.html">Basement-controlled multiple slope collapses, Rockall Bank Slide Complex, NE Atlantic</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Aggeliki Georgiopoulou&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Aggeliki Georgiopoulou,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Patrick M. 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reinforcements along them coated steel, the system to a modular base (modular system) for securing of bank slopes and slopes</a> <b>[P]</b> . <span> 外国专利：  DE202015004422U1 </span> <span> . 2015-07-14</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：性质由沿涂层钢的增强材料组成，系统固定至模块化基座（模块化系统），用于固定岸坡和斜坡 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130433674883.html">MULTIPLEX TRANSMISSION APPARATUS, TIMING SYNCHRONIZING CIRCUIT FOR MULTIPLEX TRANSMISSION APPARATUS, AND CARRIER PHASE SYNCHRONIZING CIRCUIT, MULTIPLEX TRANSMISSION METHOD, AND TIMING SYNCHRONIZING METHOD OF MULTIPLEX TRANSMISSION METHOD, AND CARRIER PHASE SYNCHRONIZING METHOD</a> <b>[P]</b> . <span> 外国专利：  JP2007325071A </span> <span> . 2007-12-13</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: 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