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Velocity models and hypocenter relocations for the Charlevoix Seismic Zone

机译：Charlevoix地震区的速度模型和低速度重新定位

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Abstract > Three‐dimensional <fi>P</fi> and <fi>S</fi> wave velocity ( <fi>V</fi> <sub> <fi>p</fi> </sub> and <fi>V</fi> <sub> <fi>s</fi> </sub> ) models and hypocenter relocations are determined for the Charlevoix Seismic Zone (CSZ) using local arrival time tomography. The CSZ is located along the St. Lawrence River about 100?km downstream from Quebec City, Canada, and is one of the most active seismic zones in eastern North America. Earthquakes occur in Grenvillian basement rocks affected by Iapetan Ocean rifting and a large Devonian meteor impact. Low <fi>V</fi> <sub> <fi>p</fi> </sub> and <fi>V</fi> <sub> <fi>s</fi> </sub> are associated with the impact structure to a depth of 12?km. Relocated hypocenters form a semicircle delineating the eastern margin of the impact structure. Northeast of the impact, hypocenters cluster into two groups separated by a region of high <fi>V</fi> <sub> <fi>p</fi> </sub> and <fi>V</fi> <sub> <fi>s</fi> </sub> velocity. Hypocenters within each group align along planar surfaces, suggesting the presence of distinct seismogenic faults. The planes trend NE, in the same direction as the Iapetan rift faults, and dip to the SE. One plane is located beneath the north shore of the St. Lawrence River and extends to a depth of at least 30?km. Two other planes with shallower dips are located beneath the river and extend to depths of 12 and 15?km. All three planes are disrupted within the impact zone but can be followed, suggesting partial preservation of rift‐parallel fault fabric. </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> >三维<fi> p </ fi>和<fi> s </ fi>波速（<fi> v </ fi> <sub> <fi> p </ fi> </ sub>和<fi> v </ fi> <sub> <fi> s </ fi> </ sub>）模型和低速度重新定位使用当地到达时间断层扫描来确定Charlevoix地震区（CSZ）。 CSZ沿着圣劳伦斯河沿着加拿大魁北克市下游约100厘米，是北美东部最活跃的地震区之一。地震发生在由IAPETAN海洋河流影响的Grenvillian地下室岩石和大型牧人流星撞击影响。低<fi> v </ fi> <sub> <fi> p </ fi> </ sub>和<fi> v </ fi> <sub> <fi> s </ fi> </ sub>相关联带有冲击结构的深度为12 km。重新定位的效率形成一个半圆形，描绘了冲击结构的东部边缘。撞击的东北部，斜置转换器聚集成两组分隔高<fi> v </ fi> <sub> <fi> p </ fi> </ sub>和<fi> v </ fi> <sub > <fi> s </ fi> </ sub>速度。每组内的低缩进者沿着平面表面对齐，表明存在不同的发酵膜。平面趋势NE，与IAPETAN RIFT断层相同，并倾向于SE。一架飞机位于圣劳伦斯河的北岸下方，延伸到至少30 km的深度。沿河下方的另外两个平面位于河下方，延伸到12和15 km的深度。所有三个平面都在冲击区内破坏，但可以遵循，表明部分保存裂缝平行故障面料。 </ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2017年第8期</span><b style="margin: 0 2px;">|</b><span>共18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=Powell Christine A.&option=202" target="_blank" rel="nofollow">Powell Christine A.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lamontagne Maurice&option=202" target="_blank" rel="nofollow">Lamontagne Maurice;</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>Center for Earthquake Research and InformationUniversity of MemphisMemphis Tennessee USA;</p> <p>Geological Survey of CanadaOttawa Ontario Canada;</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=seismotectonics&option=203" rel="nofollow">seismotectonics;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=tomography&option=203" rel="nofollow">tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=hypcenters&option=203" rel="nofollow">hypcenters;</a> </p> <div class="translation"> 机译：地震术;断层扫描;Hypenters; </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/0704020651403.html">Velocity models and hypocenter relocations for the Charlevoix Seismic Zone</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Powell Christine A.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Powell Christine A.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Lamontagne Maurice&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Lamontagne Maurice </a> <a href="/journal-foreign-34656/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of Geophysical Research. 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