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Evolution of submarine eruptive activity during the 2011–2012 EE l HH ierro event as documented by hydroacoustic images and remotely operated vehicle observations

机译:2011 - 2012年潜艇爆发活动的演变 E e L. h h 由水声图像和远程操作的车辆观测记录的IERRO事件

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Abstract >Submarine volcanic eruptions are frequent and important events, yet they are rarely observed. Here we relate bathymetric and hydroacoustic images from the 2011 to 2012 El Hierro eruption with surface observations and deposits imaged and sampled by ROV. As a result of the shallow submarine eruption, a new volcano named Tagoro grew from 375 to 89 m depth. The eruption consisted of two main phases of edifice construction intercalated with collapse events. Hydroacoustic images show that the eruptions ranged from explosive to effusive with variable plume types and resulting deposits, even over short time intervals. At the base of the edifice, ROV observations show large accumulations of lava balloons changing in size and type downslope, coinciding with the area where floating lava balloon fallout was observed. Peaks in eruption intensity during explosive phases generated vigorous bubbling at the surface, extensive ash, vesicular lapilli and formed high‐density currents, which together with periods of edifice gravitational collapse, produced extensive deep volcaniclastic aprons. Secondary cones developed in the last stages and show evidence for effusive activity with lava ponds and lava flows that cover deposits of stacked lava balloons. Chaotic masses of heterometric boulders around the summit of the principal cone are related to progressive sealing of the vent with decreasing or variable magma supply. Hornitos represent the final eruptive activity with hydrothermal alteration and bacterial mats at the summit. Our study documents the distinct evolution of a submarine volcano and highlights the range of deposit types that may form and be rapidly destroyed in such eruptions. </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> >潜艇火山爆发是频繁和重要的事件,但它们很少观察到。在这里,我们将来自2011年至2012年EL Hierro爆发的沐浴和水声图像与ROV成像和取样的表面观察和沉积物。由于浅层潜艇爆发,一个名为Tagoro的新火山增长375至89米深度。喷发包括与折叠事件相插的大厦建筑的两个主要阶段。水声图像显示爆发从爆炸性的爆炸性与可变羽流类型和产生的沉积物,即使在短时间间隔中也是如此。在大厦的基础上,ROV观察结果显示了熔岩气球的大大累积,随着观察到浮动熔岩气球辐射的区域。爆炸阶段爆发强度的峰在表面,广泛的灰,囊泡锂菌和形成的高密度电流中产生了剧烈的鼓泡,其与大厦重力崩溃的时期一起产生了广泛的深火山弹性围裙。在最后一个阶段开发的次要锥体,并显示熔岩池塘和熔岩流动的浮动活动的证据,覆盖堆积熔岩气球的沉积物。主要锥体峰会周围的异常巨石的混沌质量与通风口的逐步密封有关,减少或可变的岩浆供应。霍尼托斯代表最终喷发活性,在峰会上具有水热改变和细菌垫。我们的研究记录了潜艇火山的独特演变,并突出了可能形成的存款类型范围,并在这种爆发中迅速销毁。</ 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8期</span><b style="margin: 0 2px;">|</b><span>共29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=Somoza L.&option=202" target="_blank" rel="nofollow">Somoza L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=González F. J.&option=202" target="_blank" rel="nofollow">González F. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barker S. J.&option=202" target="_blank" rel="nofollow">Barker S. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Madureira P.&option=202" target="_blank" rel="nofollow">Madureira P.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Medialdea T.&option=202" target="_blank" rel="nofollow">Medialdea T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=de Ignacio C.&option=202" target="_blank" rel="nofollow">de Ignacio C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Louren?o N.&option=202" target="_blank" rel="nofollow">Louren?o N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=León R.&option=202" target="_blank" rel="nofollow">León R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Vázquez J. T.&option=202" target="_blank" rel="nofollow">Vázquez J. T.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Palomino D.&option=202" target="_blank" rel="nofollow">Palomino D.;</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>Marine Geology Dv.Geological Survey of Spain (IGME)Madrid Spain;</p> <p>Marine Geology Dv.Geological Survey of Spain (IGME)Madrid Spain;</p> <p>School of EnvironmentUniversity of AucklandAuckland New Zealand;</p> <p>Estrutura de Miss?o para a Extens?o da Plataforma Continental Portugal/Dpt. Geociências e ICTUniv. évoraR. Rom?o Ramalho Portugal;</p> <p>Marine Geology Dv.Geological Survey of Spain (IGME)Madrid Spain;</p> <p>Petrology Dpt. Facultad Ciencias GeológicasUniversidad ComplutenseMadrid Spain;</p> <p>Instituto Português do Mar e da AtmosferaLisboa Portugal;</p> <p>Marine Geology Dv.Geological Survey of Spain (IGME)Madrid Spain;</p> <p>Instituto Espa?ol de OceanografíaFuengirola Málaga Spain;</p> <p>Instituto Espa?ol de OceanografíaFuengirola Málaga Spain;</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=submarine&option=203" rel="nofollow">submarine;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=volcanoes&option=203" rel="nofollow">volcanoes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hotspots&option=203" rel="nofollow">hotspots;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ROV&option=203" rel="nofollow">ROV;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hydroacoustic&option=203" rel="nofollow">hydroacoustic;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=multibeam&option=203" rel="nofollow">multibeam;</a> </p> <div class="translation"> 机译:潜艇;火山;热点;ROV;水声学;多阵线; </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/0704023360396.html">Evolution of submarine eruptive activity during the 2011–2012 <fc >E</fc>E l <fc >H</fc>H ierro event as documented by hydroacoustic images and remotely operated vehicle observations</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Somoza L.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Somoza L.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=González F. 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target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 张在爱</a> <span> . 2014</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061204100292.html">车辆与NFC移动设备通信的方法及其系统、车外NFC模块</a> <b>[P]</b> . <span> 中国专利: CN111629353B </span> <span> . 2020.11.13</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120104200617.html">经由NFC将数字车辆密钥分配给无源NFC装置的系统和方法</a> <b>[P]</b> . <span> 中国专利: CN111182494A </span> <span> . 2020-05-19</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130437615153.html">u00fcberfu00fchrungseinrichtung for the beginning of a folienbahn or a folienrestgitters a thermoformmaschine to schneidmu00fchle and procedures to operate the u00fcberfu00fchrungseinrichtung</a> <b>[P]</b> . <span> 外国专利: <!-- --> AT307673T </span> <span> . 2005-11-15</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:前期为叶形火车或叶面固定器,**的热成型机械到施耐德®和操作步骤。 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130436582439.html">u00fcberfu00fchrungseinrichtung for the beginning of a folienbahn or a folienrestgitters a thermoformmaschine to schneidmu00fchle and procedures to operate the u00fcberfu00fchrungseinrichtung</a> <b>[P]</b> . <span> 外国专利: <!-- 德国专利: --> DE502004000113D1 </span> <span> . 2005-12-01</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:前期为叶形火车或叶面固定器的涂装,都需要一个热成型机到施耐德®以及操作 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130421749852.html">process for operating at least one u00fcberschalldu00fcse in a metallurgical vessel, method of determining a druckverlusts,system of 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