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首页> 外文期刊>Journal of geophysical research. Solid earth: JGR >The CECE 1303 Hongdong Earthquake and the Huoshan Piedmont Fault, Shanxi Graben: Implications for Magnitude Limits of Normal Fault Earthquakes
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The CECE 1303 Hongdong Earthquake and the Huoshan Piedmont Fault, Shanxi Graben: Implications for Magnitude Limits of Normal Fault Earthquakes

机译： ce ce 1303洪东地震和惠山皮埃蒙特断层，山西Graben：对正常故障地震的幅度限制的影响

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Abstract >The CE 1303 Hongdong earthquake, with ~270,000 deaths, has been suggested as the first magnitude 8 earthquake recorded in North China. We use 31 AMS‐14C ages to date earthquakes recorded in the Huoshan Piedmont Fault, which is interpreted to be the causative fault for the event. We interpret fault traces and map the Hongdong earthquake surface rupture in detail. Four events are identified with timings constrained at 1,060–590?year BP (corresponding to the Common Era 1303 event), 3,310–3,210?year BP, 5,460–5,380?year BP, and 26,380?year BP, respectively. The later three events have a recurrence interval of ~2,000–3,000 years. We find that the Hongdong earthquake had a rupture length of ~98?km, a maximum throw of 5.0?m and a best estimate for magnitude in the range Mw 7.2–7.6. We suggest that previous magnitude estimates are overestimates. Normal fault earthquakes have smaller upper limits to their magnitudes than thrusts, because their relatively steep dips produce intersections at the base of the seismogenic layer at smaller downdip widths than gently dipping thrust faults. The Hongdong event was not an exception to this pattern. The historic released seismic moment may be closer to the accumulated moment than previously calculated. </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”> <title type =“main”>抽象</ title> > CE 1303 Hongdong地震，〜270,000人死亡，已被提出为第一级8地震记录在华北地区。我们使用31 AMS-14C年龄达到惠山Piedmont断层的枣地震，这被解释为事件的致命因素。我们详细解释了故障迹线并映射洪洞地震表面破裂。 4个事件以1,060-590？年BP（对应于共同时代1303事件），3,310-3,210？年BP，5,460-5,380？年BP和26,380岁，分别为26,380岁，分别为26,380？后来的三个事件的复发间隔〜2,000-3,000年。我们发现红东地震的破裂长度〜98 km，最大抛出5.0？m，最佳估计在MW 7.2-7.6范围内。我们建议以前的幅度估计是高估的。正常故障地震对它们的幅度具有比推力更小的上限，因为它们的相对陡峭的浸渍在较小的下屑宽度下在较小的下倾斜宽度下产生在发泻层的底部的交叉。洪洞活动并不是这种模式的例外。历史性释放的地震时刻可能比以前计算的累积时刻更接近累积的时刻。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第4期</span><b style="margin: 0 2px;">|</b><span>共24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=Xu Yueren&option=202" target="_blank" rel="nofollow">Xu Yueren;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=He Honglin&option=202" target="_blank" rel="nofollow">He Honglin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Qidong&option=202" target="_blank" rel="nofollow">Deng Qidong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Allen Mark B.&option=202" target="_blank" rel="nofollow">Allen Mark B.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Haoyue&option=202" target="_blank" rel="nofollow">Sun Haoyue;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bi Lisi&option=202" target="_blank" rel="nofollow">Bi Lisi;</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>Key Laboratory of Active Tectonics and VolcanoInstitute of Geology China Earthquake AdministrationBeijing China;</p> <p>Key Laboratory of Active Tectonics and VolcanoInstitute of Geology China Earthquake AdministrationBeijing China;</p> <p>Key Laboratory of Active Tectonics and VolcanoInstitute of Geology China Earthquake AdministrationBeijing China;</p> <p>Department of Earth SciencesUniversity of DurhamDurham UK;</p> <p>Key Laboratory of Active Tectonics and VolcanoInstitute of Geology China Earthquake AdministrationBeijing China;</p> <p>Key Laboratory of Earthquake Monitoring and Disaster Mitigation TechnologyEarthquake Administration of Guangdong ProvinceGuangzhou China;</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=1303 Hongdong earthquake&option=203" rel="nofollow">1303 Hongdong earthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=paleoearthquake&option=203" rel="nofollow">paleoearthquake;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=normal fault&option=203" rel="nofollow">normal fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=North China&option=203" rel="nofollow">North China;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huoshan Piedmont Fault&option=203" rel="nofollow">Huoshan Piedmont Fault;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Shanxi Graben&option=203" rel="nofollow">Shanxi Graben;</a> </p> <div class="translation"> 机译：1303 hong懂earthquake;PA Leo earthquake;normal fault;north China;hu o山Piedmont fault;S焊锡GR啊Ben; </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/0704025591297.html">The <sc >CE</sc>CE 1303 Hongdong Earthquake and the Huoshan Piedmont Fault, Shanxi Graben: Implications for Magnitude Limits of Normal Fault Earthquakes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Yueren&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Xu Yueren,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=He Honglin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">He Honglin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Deng Qidong&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Deng Qidong,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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<a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=赵纪东&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 赵纪东</a> <span> <a href="/journal-cn-4935/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 国际地震动态 </a> </span> <span> . 2017</span><span>,第011期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-65536_thesis/020222950671.html">基于静力法的UBC 1997与ASCE 7-10标准水平地震作用比较</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=LIU Tianying&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . LIU Tianying</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘天英&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘天英</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=CUI Lei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,CUI Lei</a> <span> <a href="/conference-cn-65536/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2017“电力土建转型与发展”学术交流会 </a> <span> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/06130447303203.html">EARTHQUAKE PREDICTING METHOD USING EARTHQUAKE GENERATION TIME, EARTHQUAKE SOURCE POSITION AND EARTHQUAKE MAGNITUDE VALUE USING SEISMOGRAPH FOR MEASUREMENT OF VIBRATION OF EARTH</a> <b>[P]</b> . <span> 外国专利： <!-- 日本专利： --> JP2002296355A </span> <span> . 2002-10-09</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: 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