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首页> 外文期刊>Geochemistry, geophysics, geosystems >The Evolution of the Silver Hills Volcanic Center, and Revised 4040 Ar/ 3939 Ar Geochronology of Montserrat, Lesser Antilles, With Implications for Island Arc Volcanism
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The Evolution of the Silver Hills Volcanic Center, and Revised 4040 Ar/ 3939 Ar Geochronology of Montserrat, Lesser Antilles, With Implications for Island Arc Volcanism

机译:银山火山中心的演变,并修改 40 40 ar / 39 39 蒙特塞拉特,较小的安妥尔斯的AR地理学,对岛弧火山的影响

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Abstract > Studying the older volcanic centers on Montserrat, Centre Hills and Silver Hills, may reveal how volcanic activity can change over long time periods (≥1 Myr), and whether the recent activity at the Soufrière Hills is typical of volcanism throughout Montserrat's history. Here we present the first detailed mapping of the Silver Hills, the oldest and arguably least studied volcanic center on Montserrat. Volcanism at the Silver Hills was dominated by episodic andesite lava dome growth and collapse, produced Vulcanian style eruptions, and experienced periodic sector collapse events, similar to the style of volcanic activity that has been documented for the Centre Hills and Soufrière Hills. We also present an updated geochronology of volcanism on Montserrat, by revising existing ages and obtaining new 40 Ar/ 39 Ar dates and paleomagnetic ages from marine tephra layers. We show that the centers of the Silver, Centre, and Soufrière Hills were active during at least ~2.17–1.03 Ma, ~1.14–0.38 Ma, and ~0.45 Ma to present, respectively. Combined with timings of volcanism on Basse‐Terre, Guadeloupe, these ages suggest that ~0.5–1 Ma is a common lifespan for volcanic centers in the Lesser Antilles. These new dates identify a previously unrecognized overlap in activity between the different volcanic centers, which appears to be a common phenomenon in island arcs. We also identify an older stage of Soufrière Hills activity ~450–290 ka characterized by the eruption of hornblende‐orthopyroxene‐phyric lavas, demonstrating that the petrology of the Soufrière Hills eruptive products has changed at least twice throughout the volcano's development. </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> > 研究蒙特塞拉特(Center Hills和Silver Hill)上的旧火山中心可能会透露火山的活动如何在长期时间(≥1MYR),以及Soufrière山最近的活动是蒙特塞拉特历史的典型火山。在这里,我们展示了银丘斯的第一个详细的映射,最古老,最重要的是蒙特塞拉特的火山中心。银丘陵的火山主义是由情节化的熔岩圆顶增长和崩溃,产生的ulcanian风格爆发,以及经验丰富的周期性部门崩溃事件,类似于为中心山丘和Soufrière山上记录的火山活动的风格。我们还通过修改现有年龄并获得新的蒙特塞拉特对蒙特塞拉特的火山主义的更新地理学论 40 </ sup> ar / 39 </ sup> 来自海洋tephra层的AR日期和古磁性古代。我们展示了银,中心和Soufrière山的中心在至少〜2.17-1.03 mA,〜1.14-0.38 mA,〜0.45 mA至左右。这些年龄段建议〜0.5-1MA在较小的安妥尔斯中对火山中心的常见寿命,结合了巴斯凯 - ··泰尔(Basse-Terre)的时间。这些新的日期识别不同火山中心之间的活动中的先前无法识别的重叠,这似乎是岛弧中的常见现象。我们还确定了Soufrière山的较旧阶段〜450-290 Ka,其特征是由角壮的垂直藻类山脉喷发,表明Soufrière山的岩石爆发产品在整个火山的发展中发生了两次。 </ 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26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=Hatter S. J.&option=202" target="_blank" rel="nofollow">Hatter S. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Palmer M. R.&option=202" target="_blank" rel="nofollow">Palmer M. R.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gernon T. M.&option=202" target="_blank" rel="nofollow">Gernon T. M.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Taylor R. N.&option=202" target="_blank" rel="nofollow">Taylor R. N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Cole P. D.&option=202" target="_blank" rel="nofollow">Cole P. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Barfod D. N.&option=202" target="_blank" rel="nofollow">Barfod D. N.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Coussens M.&option=202" target="_blank" rel="nofollow">Coussens M.;</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>School of Ocean and Earth Science National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>School of Ocean and Earth Science National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>School of Ocean and Earth Science National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>School of Ocean and Earth Science National Oceanography CentreUniversity of SouthamptonSouthampton UK;</p> <p>School of Geography Earth and Environmental SciencesPlymouth University Drake CircusPlymouth UK;</p> <p>Scottish Universities Environmental Research CentreEast Kilbride UK;</p> <p>School of Ocean and Earth Science National Oceanography CentreUniversity of SouthamptonSouthampton UK;</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=Montserrat&option=203" rel="nofollow">Montserrat;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=40 Ar/ 39 Ar geochronology&option=203" rel="nofollow">40 Ar/ 39 Ar geochronology;</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> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=island arcs&option=203" rel="nofollow">island arcs;</a> </p> <div class="translation"> 机译:蒙特塞拉特;40 AR / 39 AR地理学;较小的安妥尔斯;岛弧; </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> </ul> </div> <div class="similarity_details"> <ul > <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704023360371.html">The Evolution of the Silver Hills Volcanic Center, and Revised <sup >4040 Ar/ <sup >3939 Ar Geochronology of Montserrat, Lesser Antilles, With Implications for Island Arc Volcanism</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hatter S. 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