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首页> 外文期刊>Geophysical Research Letters >Insights Into Fault‐Magma Interactions in an Early‐Stage Continental Rift From Source Mechanisms and Correlated Volcano‐Tectonic Earthquakes
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Insights Into Fault‐Magma Interactions in an Early‐Stage Continental Rift From Source Mechanisms and Correlated Volcano‐Tectonic Earthquakes

机译:从源机制和相关的火山构造地震中,在早期大陆裂谷中洞察故障岩浆互动

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Abstract > Strain in magmatic rifts is accommodated by both faulting and dike intrusion, but little is known of the frequency of dike intrusions in early‐stage rifts. We use a new earthquake data set from a dense temporary seismic array (2013–2014) in the ~7‐Myr‐old Magadi‐Natron‐Manyara section of the East African Rift, which includes the carbonatitic Oldoinyo Lengai volcano that erupted explosively in 2007–2008. Full moment tensor analyses were performed on M ??3.4 earthquakes (0.03‐ to 0.10‐Hz band) that occurred during the intereruptive cycle. We find two opening crack‐type and various non‐double‐couple earthquake source mechanisms and interpret these as fluid‐involved fault rupture. From waveform analysis on the nearest permanent seismic station, we conclude that similar rupture processes probably occur over eruptive and intereruptive cycles. The repeated and dynamically similar fluid‐involved seismicity, along with intrabasinal localization of active deformation, suggests that significant and persistent strain is accommodated by magmatic processes, modulated by tectonic cycles. </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”XML:Lang =“en”> <标题类型=“main”>抽象</ title> >岩浆裂缝中的应变通过故障和堤防入侵,但很少是已知的早期裂缝中堤防入侵的频率。我们在东非Rift的〜7 Myr-Old Magadi-Natron-Moreara部分中使用了从密集的临时地震阵列(2013-2014)的新地震数据,其中包括2007年爆炸性爆炸的碳酸扎古妮廷兰台火山-2008。全时刻张量分析在 m </ i>上进行?3.4在间相循环期间发生的地震(0.03至0.10-Hz波段)。我们发现两种开放式裂缝类型和各种非双夫夫夫妇地震源机构,并将其解释为流体涉及的故障破裂。从最近的永久地震站的波形分析,我们得出结论,类似的破裂过程可能发生爆发和共振循环。重复和动态类似的流体涉及的液相性以及内部主动变形的内部定位表明,通过构造循环调节的岩浆工艺,可以容纳显着和持久的菌株。 </ p> </ abstract> </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-23539/'>《Geophysical Research Letters》</a> <b style="margin: 0 2px;">|</b><span>2019年第4期</span><b style="margin: 0 2px;">|</b><span>共10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=Oliva S. J.&option=202" target="_blank" rel="nofollow">Oliva S. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ebinger C. J.&option=202" target="_blank" rel="nofollow">Ebinger C. J.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wauthier C.&option=202" target="_blank" rel="nofollow">Wauthier C.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Muirhead J. D.&option=202" target="_blank" rel="nofollow">Muirhead J. D.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Roecker S. W.&option=202" target="_blank" rel="nofollow">Roecker S. W.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Rivalta E.&option=202" target="_blank" rel="nofollow">Rivalta E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Heimann S.&option=202" target="_blank" rel="nofollow">Heimann S.;</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>Tulane UniversityNew Orleans LA USA;</p> <p>Tulane UniversityNew Orleans LA USA;</p> <p>Pennsylvania State UniversityUniversity Park PA USA;</p> <p>Syracuse UniversitySyracuse NY USA;</p> <p>Rensselaer Polytechnic InstituteTroy NY USA;</p> <p>GFZ German Centre for GeosciencesPotsdam Germany;</p> <p>GFZ German Centre for GeosciencesPotsdam 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=full moment tensor&option=203" rel="nofollow">full moment tensor;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=non‐double‐couple&option=203" rel="nofollow">non‐double‐couple;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=magma‐related faulting&option=203" rel="nofollow">magma‐related faulting;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=East Africa rift&option=203" rel="nofollow">East Africa rift;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=source mechanism&option=203" rel="nofollow">source mechanism;</a> </p> <div class="translation"> 机译:完整时刻张量;非双夫妇;岩浆相关的断层;东非裂缝;源机制; </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/0704019852546.html">Insights Into Fault‐Magma Interactions in an Early‐Stage Continental Rift From Source Mechanisms and Correlated Volcano‐Tectonic Earthquakes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Oliva S. 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