首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >Mixed‐Mode Slip Behavior of the Altotiberina Low‐Angle Normal Fault System (Northern Apennines, Italy) through High‐Resolution Earthquake Locations and Repeating Events
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Mixed‐Mode Slip Behavior of the Altotiberina Low‐Angle Normal Fault System (Northern Apennines, Italy) through High‐Resolution Earthquake Locations and Repeating Events

机译:通过高分辨率地震位置和重复事件,Altotiberina低角度正常故障系统(意大利北极山脉)的混合模式滑动行为

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Abstract > We generated a 4.5‐year‐long (2010–2014) high‐resolution earthquake catalogue, composed of ~37,000 events with <fi>M</fi> <sub> <fi>L</fi> </sub> ?<?3.9 and <fi>M</fi> <sub> <fi>C</fi> </sub> ?=?0.5 completeness magnitude, to report on the seismic activity of the Altotiberina (ATF) low‐angle normal fault system and to shed light on the mechanical behavior and seismic potential of this fault, which is capable of generating a <fi>M</fi> 7 event. Seismicity defines the geometry of the fault system composed of the low‐angle (15°–20°) ATF, extending for ~50?km along strike and between 4 and 16?km at depth showing an ~1.5?km thick fault zone made of multiple subparallel slipping planes, and a complex network of synthetic/antithetic higher‐angle segments located in the ATF hanging wall (HW) that can be traced along strike for up to 35?km. Ninety percent of the recorded seismicity occurs along the high‐angle HW faults during a series of minor, sometimes long‐lasting (months) seismic sequences with multiple <fi>M</fi> <sub> <fi>W</fi> </sub> 3+ mainshocks. Remaining earthquakes ( <fi>M</fi> <sub> <fi>L</fi> </sub> ?<?2.4) are released instead along the low‐angle ATF at a constant rate of ~2.2 events per day. Within the ATF‐related seismicity, we found 97 clusters of repeating earthquakes (RE), mostly consisting of doublets occurring during short interevent time (hours). RE are located within the geodetically recognized creeping portions of the ATF, around the main locked asperity. The rate of occurrence of RE seems quite synchronous with the ATF‐HW seismic release, suggesting that creeping may guide the strain partitioning in the ATF system. The seismic momen </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> >我们生成了4.5年长(2010-2014)高分辨率地震目录,用<fi> m </ fi> <sub> <fi> l </ sub> </ sub> <x?3.9和<fi> <fi> <sub> <fi> c < / fi> </ sub>?=?0.5完整性幅度,报告Altotiberina(ATF)低角度正常故障系统的地震活动,并阐明了这种故障的机械行为和地震潜力,有能力生成<fi> m </ fi> 7事件。地震性定义了由低角度(15°-20°)ATF组成的故障系统的几何形状,沿着撞击延伸〜50Ωkm,深度延伸到4到16 km,显示为〜1.5Ω·km厚的断层区域多个子平行滑动平面,以及位于ATF悬挂墙(HW)中的合成/抗静性高角段的复杂网络,其可以沿着撞击追踪到达35 km。九十百分之九十的沿着高角度HW故障发生在一系列次要,有时长的(几个月)地震序列中,具有多个<fi> m </ fi> <sub> <fi> w </ fi> </ sub> 3+ mainshocks。剩余地震(<fi> m </ fi> <sub> <fi> l </ fi> </ sub> <cu> </ sub> <Δ2.4)沿着低角度的atf以〜2.2每天的恒定速率释放。在与ATF相关的地震内,我们发现了97个重复地震(RE)的簇,主要由在短时间内(小时)发生的双峰组成。 Re位于ATF的地理上公认的爬行部分内,周围主要锁定粗糙。 RE似乎与ATF-HW地震释放的发生率非常同步,表明爬行可以引导菌株分区在ATF系统中。地震莫伦 </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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共21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=Valoroso Luisa&option=202" target="_blank" rel="nofollow">Valoroso Luisa;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chiaraluce Lauro&option=202" target="_blank" rel="nofollow">Chiaraluce Lauro;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Di Stefano Raffaele&option=202" target="_blank" rel="nofollow">Di Stefano Raffaele;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Monachesi Giancarlo&option=202" target="_blank" rel="nofollow">Monachesi Giancarlo;</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>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</p> <p>Istituto Nazionale di Geofisica e VulcanologiaRome Italy;</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=low‐angle normal faults&option=203" rel="nofollow">low‐angle normal faults;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=high‐resolution earthquake locations&option=203" rel="nofollow">high‐resolution earthquake locations;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Northern Apennines&option=203" rel="nofollow">Northern Apennines;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=repeating earthquakes&option=203" rel="nofollow">repeating earthquakes;</a> </p> <div class="translation"> 机译:低角度正常断层;高分辨率的地震位置;北亚平宁山脉;重复地震; </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/0704025592995.html">Mixed‐Mode Slip Behavior of the Altotiberina Low‐Angle Normal Fault System (Northern Apennines, Italy) through High‐Resolution Earthquake Locations and Repeating Events</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Valoroso Luisa&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Valoroso Luisa,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chiaraluce Lauro&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chiaraluce Lauro,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Di Stefano Raffaele&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Di Stefano Raffaele,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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