Gravity‐Driven Deposits in an Active Margin (Ionian Sea) Over the Last 330,000 Years

K?ng Eléonore; Zaragosi Sébastien; Schneider Jean‐Luc; Garlan Thierry; Bachèlery Patrick; Sabine Marjolaine; San Pedro Laurine

摘要

Abstract >In the Ionian Sea, the subduction of the Nubia plate underneath the Eurasia plate leads to an important sediment remobilization on the Calabrian Arc and the Mediterranean Ridge. These events are often associated with earthquakes and tsunamis. In this study, we analyze gravity‐driven deposits in order to establish their recurrence time on the Calabrian Arc and the western Mediterranean Ridge. Four gravity cores collected on ridges and slope basins of accretionary prisms record turbidites, megaturbidites, slumping and micro‐faults over the last 330,000 years. These turbidites were dated by correlation with a hemipelagic core with a multi‐proxy approach: radiometric dating, δ18O, b* colour curve, sapropels and tephrochronology. The origin of the gravity‐driven deposits was studied with a sedimentary approach: grain‐size, lithology, thin section, geochemistry of volcanic glass. The results suggest three periods of presence/absence of gravity‐driven deposits: a first on the western lobe of the Calabrian Arc between 330,000 and 250,000 years, a second between 120,000 years and present day on the eastern lobe of the Calabrian Arc and over the last 60,000 years on the western lobe, and a third on the Mediterranean Ridge over the last 37,000 years. Return times for gravity‐driven deposits are around 1,000 years during the most important record periods. The turbidite activity also highlights the presence of volcaniclastic turbidites that seems to be link to the Etna changing morphology over the last 320,000 years. </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”> <标题类型=“main”>抽象</ title> >在爱奥尼亚海中，欧亚邦德下面的Nubia板的俯冲导致Calabrian弧和地中海山脊上的重要沉积物。这些事件通常与地震和海啸有关。在这项研究中，我们分析了重力驱动的存款，以便在Calabrian弧和西部地中海山脊上建立其复发时间。收集的四个重力核心在过去330,000年里，射击棱镜的山脊和坡盆地记录浊度，Megaturbidites，坍塌和微漏。通过与多代理方法的六骨芯相关的相关性，通过多功能方法：辐射测定，Δ18O，b *颜色曲线，sapropels和tephrochronology。用沉积方法研究了重力驱动沉积物的起源：晶粒尺寸，岩性，薄剖面，火山玻璃的地球化学。结果表明了三次存在/缺乏重力驱动的沉积物：卡拉巴舞的西叶的第一个在330,000和25万年之间，一秒就在Calabrian弧的东叶的120,000年和现在。在过去的37,000年里，西叶上的最近60,000年，在地中海山脊上是第三年。重力驱动存款的返回时间在最重要的记录期内大约1,000年。浊度活性也突出了火山的存在，似乎是在过去320,000年内与Etna改变形态的链接。</ 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>2017年第11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=K?ng Eléonore&option=202" target="_blank" rel="nofollow">K?ng Eléonore;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zaragosi Sébastien&option=202" target="_blank" rel="nofollow">Zaragosi Sébastien;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Schneider Jean‐Luc&option=202" target="_blank" rel="nofollow">Schneider Jean‐Luc;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Garlan Thierry&option=202" target="_blank" rel="nofollow">Garlan Thierry;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bachèlery Patrick&option=202" target="_blank" rel="nofollow">Bachèlery Patrick;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sabine Marjolaine&option=202" target="_blank" rel="nofollow">Sabine Marjolaine;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=San Pedro Laurine&option=202" target="_blank" rel="nofollow">San Pedro Laurine;</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>EPOC UMR CNRS 5805 Université de Bordeaux allée Geoffroy Saint‐Hilaire CS 50023Pessac France;</p> <p>EPOC UMR CNRS 5805 Université de Bordeaux allée Geoffroy Saint‐Hilaire CS 50023Pessac France;</p> <p>EPOC UMR CNRS 5805 Université de Bordeaux allée Geoffroy Saint‐Hilaire CS 50023Pessac France;</p> <p>SHOM/DOPS/HOM/Sédimentologie 13 rue du Chatellier CS 92803Brest France;</p> <p>LMV/OPGC Université Blaise Pascal de Clermont‐Ferrand Campus des Cézeaux 6 avenue Blaise Pascal TSA60026 – CS60026Aubière Cedex France;</p> <p>EPOC UMR CNRS 5805 Université de Bordeaux allée Geoffroy Saint‐Hilaire CS 50023Pessac France;</p> <p>Laboratoire Domaines Océaniques UMR 6538 Université de Bretagne occidentale IUEM rue Dumont d'UrvillePlouzané France;</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=Ionian Sea&option=203" rel="nofollow">Ionian Sea;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=accretionary wedges&option=203" rel="nofollow">accretionary wedges;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=palaeoearthquakes&option=203" rel="nofollow">palaeoearthquakes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=etna volcanism&option=203" rel="nofollow">etna volcanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=natural hazard&option=203" rel="nofollow">natural hazard;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=turbidites&option=203" rel="nofollow">turbidites;</a> </p> <div class="translation"> 机译：爱奥尼亚海;痛苦的楔子;古老地震;etna火山;自然危险;浊度; </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/0704023360771.html">Gravity‐Driven Deposits in an Active Margin (Ionian Sea) Over the Last 330,000 Years</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=K?ng Eléonore&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">K?ng Eléonore,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zaragosi 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