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首页> 外文期刊>Geochemistry, geophysics, geosystems >Mud Volcanism in a Canyon: Morphodynamic Evolution of the Active Venere Mud Volcano and Its Interplay With Squillace Canyon, Central Mediterranean
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Mud Volcanism in a Canyon: Morphodynamic Evolution of the Active Venere Mud Volcano and Its Interplay With Squillace Canyon, Central Mediterranean

机译：泥泞的火山中的峡谷：主动venere泥火山的形态学演变及其与Squillace Canyon的相互作用，中部地中海

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Abstract > Submarine mud volcanoes develop through the extrusion of methane‐rich fluids and sediments onto the seafloor. The morphology of a mud volcano can record its extrusive history and processes of erosion and deformation affecting it. The study of offshore mud volcano dynamics is limited because only few have been mapped at resolutions that reveal their detailed surface structures. More importantly, rates and volumes of extruded sediment and methane are poorly constrained. The 100 m high twin cones of Venere mud volcano are situated at ～1,600 m water depth within Squillace Canyon along the Ionian Calabrian margin, Mediterranean Sea. Seafloor bathymetry and backscatter data obtained by a ship‐based system and an autonomous underwater vehicle (AUV) allow mapping of mudflow deposits of the mud volcano and bedforms in the surrounding canyon. Repeated surveying by AUV document active mud movement at the western summit in between 2014 and 2016. Through sediment coring and tephrochronology, ages of buried mudflow deposits are determined based on the sedimentation rate and the thickness of overlying hemipelagic sediments. An average extrusion rate of 27,000 m 3 /yr over the last ～882 years is estimated. These results support a three‐stage evolutionary model of Venere mud volcano since ～4,000 years ago. It includes the onset of quiescence at the eastern cone (after ～2,200 years ago), erosive events in Squillace Canyon (prior to ～882 years ago), and mudflows from the eastern cone (since ～882 years). This study reveals new interactions between a mud volcano and a canyon in the deep sea. </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> > 潜水艇泥火山通过挤出富含甲烷的液体和沉积物而发展到海底上。泥火火山的形态可以记录其侵蚀和变形的外部历史和过程。海上泥火火山动力学的研究有限，因为只有很少涂在揭示其详细表面结构的决议上。更重要的是，挤出沉积物和甲烷的速率和体积受到严重受损。 Venere Mud火山的100米高，距离Ionian Calabrian Margin，地中海沿着Ionian Calabrian Margin，位于Quilla空间峡谷的水深〜1,600米水深。由船舶系统和自主水下车辆（AUV）获得的海底沐浴浴和反向散射数据允许在周围的峡谷中绘制泥浆火山的泥浆沉积物和弯曲。 2014年至2016年间的AUV文件主动泥浆运动反复测量。通过沉积物芯片和Tephrochronologrol，基于沉降率和覆盖血管沉积物的厚度来确定埋地泥浆沉积物。平均挤出率为27,000米 3 </ sup> / Yr在过去〜882年中估计。这些结果支持自〜4000年前以来venere泥火山的三阶段进化模型。它包括东锥体的静态发作（在〜2,200年前），Squillace Canyon的腐蚀事件（在〜882年之前），以及来自东锥的泥流（自〜882年）。本研究揭示了泥火山与深海峡谷之间的新相互作用。 </ 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>2018年第2期</span><b style="margin: 0 2px;">|</b><span>共23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=Loher Markus&option=202" target="_blank" rel="nofollow">Loher Markus;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ceramicola Silvia&option=202" target="_blank" rel="nofollow">Ceramicola Silvia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wintersteller Paul&option=202" target="_blank" rel="nofollow">Wintersteller Paul;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Meinecke Gerrit&option=202" target="_blank" rel="nofollow">Meinecke Gerrit;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sahling Heiko&option=202" target="_blank" rel="nofollow">Sahling Heiko;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bohrmann Gerhard&option=202" target="_blank" rel="nofollow">Bohrmann Gerhard;</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>MARUM – Center for Marine Environmental Sciences and Faculty of GeosciencesUniversity of BremenBremen Germany;</p> <p>Istituto Nazionale di Oceanografia e di Geofisica Sperimentale ‐ OGSSgonico Trieste Italy;</p> <p>MARUM – Center for Marine Environmental Sciences and Faculty of GeosciencesUniversity of BremenBremen Germany;</p> <p>MARUM – Center for Marine Environmental Sciences and Faculty of GeosciencesUniversity of BremenBremen Germany;</p> <p>MARUM – Center for Marine Environmental Sciences and Faculty of GeosciencesUniversity of BremenBremen Germany;</p> <p>MARUM – Center for Marine Environmental Sciences and Faculty of GeosciencesUniversity of BremenBremen 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=mud volcano&option=203" rel="nofollow">mud volcano;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mud breccia&option=203" rel="nofollow">mud breccia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=AUV&option=203" rel="nofollow">AUV;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine canyon&option=203" rel="nofollow">submarine canyon;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tephra&option=203" rel="nofollow">tephra;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Calabrian Accretionary Prism&option=203" rel="nofollow">Calabrian Accretionary Prism;</a> </p> <div class="translation"> 机译：泥火山;泥毛菌;auv;潜艇峡谷;tephra;卡拉布里安accretionary prism; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360392.html">Mud Volcanism in a Canyon: Morphodynamic Evolution of the Active Venere Mud Volcano and Its Interplay With Squillace Canyon, Central Mediterranean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Loher Markus&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Loher Markus,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ceramicola Silvia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ceramicola Silvia,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wintersteller Paul&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wintersteller Paul,</a> <a href="/journal-foreign-23285/" target="_blank" rel="nofollow" class="tuijian_authcolor">Geochemistry, geophysics, geosystems .</a> <span>2018</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：泥泞的火山中的峡谷：主动venere泥火山的形态学演变及其与Squillace Canyon的相互作用，中部地中海</span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-foreign_deep-sea-research.-part-i-oceanographic-research-papers_thesis/0204112183759.html">Seafloor sealing, doming, and collapse associated with gas seeps and authigenic carbonate structures at Venere mud volcano, Central Mediterranean</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Loher Markus&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Loher Markus,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Marcon Yann&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Marcon Yann,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pape Thomas&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Pape Thomas,</a> <a href="/journal-foreign-817/" target="_blank" rel="nofollow" class="tuijian_authcolor">Deep-Sea Research .</a> <span>2018</span><span>,第JULa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：地中海中部Venere泥火山的海底密封，隆起和塌陷与天然气渗漏和自生碳酸盐结构有关</span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704024718314.html">Long-term in situ observations at the Athina mud volcano, Eastern Mediterranean: Taking the pulse of mud volcanism</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Walter Menapace&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Walter Menapace,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=David V?lker&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">David V?lker,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heiko Sahling&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Heiko Sahling,</a> <a href="/journal-foreign-30366/" target="_blank" rel="nofollow" class="tuijian_authcolor">Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth .</a> <span>2017</span><span>,第期</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：在Athina Mud火山，东地中海的长期观测：采取泥火山的脉搏</span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-conference-foreign_meeting-224110_thesis/020515518035.html">Natural Seepage Systems at Biloxi Dauphin Domes Mars Mud Volcano, North East Mississippi Canyon Protraction Area, Gulf of Mexico</a> <b>[C]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Peter D. 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