30 Years in the Life of an Active Submarine Volcano: A Time‐Lapse Bathymetry Study of the Kick‐'em‐Jenny Volcano, Lesser Antilles

Allen R. W.; Berry C.; Henstock T. J.; Collier J. S.; Dondin F. J‐Y.; Rietbrock A.; Latchman J. L.; Robertson R. E. A.

摘要

Abstract > Effective monitoring is an essential part of identifying and mitigating volcanic hazards. In the submarine environment this is more difficult than onshore because observations are typically limited to land‐based seismic networks and infrequent shipboard surveys. Since the first recorded eruption in 1939, the Kick‐'em‐Jenny (KeJ) volcano, located 8 km off northern Grenada, has been the source of 13 episodes of T‐phase signals. These distinctive seismic signals, often coincident with heightened body‐wave seismicity, are interpreted as extrusive eruptions. They have occurred with a recurrence interval of around a decade, yet direct confirmation of volcanism has been rare. By conducting new bathymetric surveys in 2016 and 2017 and reprocessing 4 legacy data sets spanning 30 years we present a clearer picture of the development of KeJ through time. Processed grids with a cell size of 5 m and vertical precision on the order of 1–4 m allow us to correlate T‐phase episodes with morphological changes at the volcano's edifice. In the time‐period of observation 7.09 × 10 6 m 3 of material has been added through constructive volcanism – yet 5 times this amount has been lost through landslides. Limited recent magma production suggests that KeJ may be susceptible to larger eruptions with longer repeat times than have occurred during the study interval, behavior more similar to sub‐aerial volcanism in the arc than previously thought. T‐phase signals at KeJ have a varied origin and are unlikely to be solely the result of extrusive submarine eruptions. Our results confirm the value of repeat swath bathymetry surveys in assessing submarine volcanic hazards. </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> > 有效的监测是识别和减轻火山危害的重要组成部分。在潜艇环境中，这比陆上更困难，因为观察通常限于陆地地震网络和不经常的船上调查。自1939年首次拍摄的爆发以来，踢球 - 吉尼（Kej）火山距离格林纳达州北部8公里，一直是T相信号的13次剧集。这些独特的地震信号通常与高度的体波地震性重合，被解释为喷发。他们已经发生了左右十年的复发间隔，但是直接确认火山主义已经很少见。通过在2016年和2017年进行新的沐浴调查，并再加工4传统数据集30年来，我们通过时间更清楚地了解了Kej的发展。电池大小为5米和垂直精度的加工网格，大约为1-4米，让我们将T相位与火山的大厦的形态变化相关联。在观察期7.09×10时期 6 </ sup> M. 3 </ sup> 通过建设性的火山主义添加了材料 - 然而，通过山体滑坡丢失了5倍。最近的最近岩浆生产表明，在研究间隔期间，kej比在研究间隔内的更长的重复时间中的爆发可能易受较大的爆发，而是与先前常见的弧形中的亚空中火山相似。在Kej处的T相位信号具有各种原点，并且不太可能是挤出潜艇喷发的结果。我们的结果证实了重复SWATH沐浴浴评估评估潜艇火山危害的价值。 </ 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3期</span><b style="margin: 0 2px;">|</b><span>共17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=Allen R. W.&option=202" target="_blank" rel="nofollow">Allen R. W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Berry C.&option=202" target="_blank" rel="nofollow">Berry C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Henstock T. J.&option=202" target="_blank" rel="nofollow">Henstock T. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Collier J. S.&option=202" target="_blank" rel="nofollow">Collier J. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Dondin F. J‐Y.&option=202" target="_blank" rel="nofollow">Dondin F. J‐Y.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rietbrock A.&option=202" target="_blank" rel="nofollow">Rietbrock A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Latchman J. L.&option=202" target="_blank" rel="nofollow">Latchman J. L.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Robertson R. E. A.&option=202" target="_blank" rel="nofollow">Robertson R. E. A.;</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>Department of Earth Science and EngineeringImperial College LondonLondon UK;</p> <p>Department of Earth Science and EngineeringImperial College LondonLondon UK;</p> <p>Ocean and Earth ScienceNational Oceanography CentreSouthampton UK;</p> <p>Department of Earth Science and EngineeringImperial College LondonLondon UK;</p> <p>UWI Seismic Research CentreSt Augustine Trinidad and Tobago;</p> <p>Geophysical InstituteKarlsruhe Institute of TechnologyKarlsruhe Germany;</p> <p>UWI Seismic Research CentreSt Augustine Trinidad and Tobago;</p> <p>UWI Seismic Research CentreSt Augustine Trinidad and Tobago;</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=time‐lapse bathymetry&option=203" rel="nofollow">time‐lapse bathymetry;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kick‐'em‐Jenny&option=203" rel="nofollow">Kick‐'em‐Jenny;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine volcanism&option=203" rel="nofollow">submarine volcanism;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=submarine landslides&option=203" rel="nofollow">submarine landslides;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lesser Antilles&option=203" rel="nofollow">Lesser Antilles;</a> </p> <div class="translation"> 机译：延时沐浴;踢 - 'jenny;潜艇山脉;潜艇山体滑坡;较小的安妥尔斯; </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/0704023360295.html">30 Years in the Life of an Active Submarine Volcano: A Time‐Lapse Bathymetry Study of the Kick‐'em‐Jenny Volcano, Lesser Antilles</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Allen R. 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Allen,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=C. Berry&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">C. Berry,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=T. J. Henstock&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">T. J. Henstock,</a> <span>2018</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：在一个活跃的潜艇火山的生活中30年：令人矛盾的巴尼火山，较小的安妥尔斯</span> </p> </li> <li> <div> <b>8. </b><a class="enjiyixqcontent" href="/ntis-science-report_pb_thesis/02071332231.html">Versatile Time-Lapse Camera System Developed by the Hawaiian Volcano Observatory for Use at Kilauea Volcano, Hawaii; Scientific investigations rept</a> <b>[R] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Orr, T. R.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Orr, T. R.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hoblitt, R. P.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hoblitt, R. P. </a> <span>2008</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：多功能延时摄像系统由夏威夷火山观测台开发，供夏威夷基拉韦厄火山使用;科学调查工作</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_recent-developments-world-seismology_thesis/0201253425258.html">1980年圣海伦斯火山爆发对之后30年火山学研究的启示</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=James W Vallance&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . James W Vallance</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cynthia A Gardner&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,Cynthia A Gardner</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=William E Scott&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,William E Scott</a> <span> <a href="/journal-cn-4935/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 国际地震动态 </a> </span> <span> . 2010</span><span>,第008期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/academic-journal-cn_geology-in-china_thesis/0201252100513.html">内蒙古科尔沁右翼中旗协和尔斯德中生代火山沉积地层时代研究</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=付俊彧&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 付俊彧</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=那福超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,那福超</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑少林&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑少林</a> <span> <a href="/journal-cn-4800/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国地质 </a> </span> <span> . 2018</span><span>,第001期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_shanghai-philately_thesis/0201229111682.html">波波卡特佩特和伊斯塔西瓦特尔火山极限片</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . </a> <span> <a href="/journal-cn-3580/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 上海集邮 </a> </span> <span> . 2012</span><span>,第008期</span> </span> </div> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/academic-journal-cn_shanghai-philately_thesis/0201229111706.html">波波卡特佩特和伊斯塔西瓦特尔火山早期极限片</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=长弓&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 长弓</a> <span> <a href="/journal-cn-3580/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 上海集邮 </a> </span> <span> . 2012</span><span>,第008期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_translated-world-seismology_thesis/0201254188111.html">由尔奈斯火山上的GEOSCOPE VBB台站得到的地倾斜信号</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=J.Battaglia&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . J.Battaglia</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭贵安&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郭贵安</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=等&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,等</a> <span> <a href="/journal-cn-5012/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 世界地震译丛 </a> </span> <span> . 2001</span><span>,第002期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-35637_thesis/020221331282.html">额尔剂斯火山岩岩浆成因的微量元素依据</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=白正华&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 白正华</a> <span> <a href="/conference-cn-35637/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国矿物学岩石学地球化学研究新进展学术交流会 </a> <span> <span> . 1994</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130422790934.html">use of artificial geysers thermoelectric constant pressure products in active volcanoes adapted to dissalare controlled amounts of saline water of the sea forcibly introduced, and converted into electrical energy the thermal energy extracted from the gayser the active volcano, p revia closure of cone volcanoes natural by means of a removable dome prefabwith openings to discharge of security.</a> <b>[P]</b> . <span> 外国专利：  IT1391731B1 </span> <span> . 2012-01-27</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：在活动火山中使用人工间歇泉热电恒压产品，以强行驱散受控量的海水中的盐水，并将从活动火山的盖瑟河中提取的热能转化为电能，通过自然方式封闭圆锥形火山带有开口的可移动圆顶预制件，以释放安全性。 </span> </p> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06130427735163.html">production of artificial geysers in active volcanoes to tarsformarne geothermal energy into electrical energy or chemicals (chain of hydrogen from steam.</a> <b>[P]</b> . <span> 外国专利：  ITCT20080013A1 </span> <span> . 2010-02-27</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：在活火山中生产人造间歇泉，将tarsformarne地热能转化为电能或化学物质（来自蒸汽的氢链。 </span> </p> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130444492299.html">wtmw system exploitation of heat from active volcanoes to produce steam</a> <b>[P]</b> . <span> 外国专利：  ITSO20020004U1 </span> <span> . 2002-12-27</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：wtmw系统利用活火山产生的热量产生蒸汽 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> 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