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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Integrated Paleoseismic Chronology of the Last Glacial Lake Lisan: From Lake Margin Seismites to Deep‐Lake Mass Transport Deposits
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Integrated Paleoseismic Chronology of the Last Glacial Lake Lisan: From Lake Margin Seismites to Deep‐Lake Mass Transport Deposits

机译：最后冰川湖Lisan的综合古摆力：来自湖泊保证金地震位到深湖大众运输沉积物

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Abstract > Seismically disturbed sedimentary sequences (seismites) in the last glacial (70–14?ka) Lisan Formation are exposed in the marginal terraces of the Dead Sea and recovered from sedimentary core drilled by the International Continental Scientific Drilling Programs at the depocenter of the lake at water depth of 300?m. The core reveals various types of centimeter‐ to meter‐scale disturbed lake sediments: turbidites, homogenites, slumps, and other deformations, interspersed with undisturbed lamination. The transported sediments comprise a main source of the thickness tripling of the Lisan Formation at the depocenter of the lake compared to the margins. Excluding (mass transport deposits MTDs) from chronology yields a normal, event‐free age‐depth model for core. Moreover, time intervals of units missing at the exposed sections of the lake margin are synchronous with intervals of mass transport deposits (MTDs) at the deepest lake floors. In the deep core, the recurrence interval range of MTD with thickness >?1?cm is ~ 100–300?years, while that of the thick MTD (>50?cm) is ~ 2,500 years, twice the recurrence interval of the seismites at the lake's margins. The ~1,000 year recurrence at the lake's margins lies within the ranges that have been calculated for ~ M 6.5–7 earthquakes. The significantly higher figure shown by depocenter core suggests activity on various faults and the response of the lake sediments in the entire Dead Sea basin. Overall, an unprecedented chronology of seismic activity was achieved for the late Pleistocene Lisan Formation providing a framework of earthquake activity in the vicinity of the Dead Sea basin during the period of the last high lake stand. </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> >最后的冰川（70-14 ka）Lisan中的地震干扰沉积序列（地震）形成在死海的边缘露台中暴露，并从湖泊的石碑，水深在300？m的水深在湖泊的国际大陆科学钻探计划中恢复了沉积核心。核心揭示了各种类型的厘米到米级扰动的湖泊沉积物：浑浊，均质，坍塌等变形，穿插着不受干扰的层压。与边缘相比，输送的沉积物包括湖泊中环戊烷中的Lisan形成的厚度三倍的主要来源。从年度学中排除（大规模运输存款MTDS）产生正常，无事件的核心Adde-Deame模型。此外，在湖泊边缘的暴露部分缺失的单位的时间间隔与最深湖地板的大规模运输沉积物（MTD）间隔是同步的。在深核中，MTD的复发间隔范围为厚度> 1？cm是〜100-300？多年，而厚的MTD（>50Ω·厘米）的〜2500年，两倍于地震物的复发间隔在湖的边缘。湖泊边缘的〜1,000年的复发位于已计算的范围内，该范围为〜 m </ i> 6.5-7地震。 Depenter Core所示的显着提高数字表明了各种故障的活动和湖泊沉积物在整个死海盆地的响应。总的来说，为晚熟活动的思想活动的前所未有的地震活动年表，在最后一次高湖站期间提供死海盆地附近的地震活动框架。 </ 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>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共19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=Kagan Elisa&option=202" target="_blank" rel="nofollow">Kagan Elisa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stein Mordechai&option=202" target="_blank" rel="nofollow">Stein Mordechai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marco Shmuel&option=202" target="_blank" rel="nofollow">Marco Shmuel;</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>Geological Survey of IsraelJerusalem Israel;</p> <p>Geological Survey of IsraelJerusalem Israel;</p> <p>Department of GeophysicsTel Aviv UniversityTel Aviv Israel;</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=paleoseismology&option=203" rel="nofollow">paleoseismology;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mass transport deposits&option=203" rel="nofollow">mass transport deposits;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lake seismites&option=203" rel="nofollow">lake seismites;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=earthquake recurrence&option=203" rel="nofollow">earthquake recurrence;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lake Lisan&option=203" rel="nofollow">Lake Lisan;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dead Sea basin&option=203" rel="nofollow">Dead Sea basin;</a> </p> <div class="translation"> 机译：古摆力;大众运输沉积物;地震湖;地震复发;丽珊湖;死海盆地; </div> </li> <li> <span class="lefttit">入库时间</span> <span>2022-08-20 09:24:19</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 >专利</li> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591486.html">Integrated Paleoseismic Chronology of the Last Glacial Lake Lisan: From Lake Margin Seismites to Deep‐Lake Mass Transport Deposits</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kagan Elisa&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Kagan Elisa,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Stein Mordechai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Stein Mordechai,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marco Shmuel&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Marco Shmuel </a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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pH-stabilization, comprises providing bicarbonate buffer and introducing gaseous carbon dioxide into deeper layers of a lake during a period of stagnation under stratified conditions</a> <b>[P]</b> . <span> 外国专利： <!-- 德国专利： --> DE102012014433A1 </span> <span> . 2014-01-23</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：用流入的酸负荷处理湖泊以保持pH值稳定，包括提供碳酸氢盐缓冲液并将分层状态下停滞期间将气态二氧化碳引入湖泊的更深层 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130448186607.html">Deep water drainage pipe for lakes with natural outflow automatically regulates outflow rate according to level of water in balancing lake</a> <b>[P]</b> . <span> 外国专利： <!-- 德国专利： --> DE10015793A1 </span> <span> . 2001-04-12</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: 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