Crustal Azimuthal Anisotropy Beneath the Central North China Craton Revealed by Receiver Functions

Zheng Tuo; Ding Zhifeng; Ning Jieyuan; Liu Kelly H.; Gao Stephen S.; Chang Lijun; Kong Fansheng; Fan Xiaoping

摘要

Abstract > To characterize crustal anisotropy beneath the central North China Craton (CNCC), we apply a recently developed deconvolution approach to effectively remove near‐surface reverberations in the receiver functions recorded at 200 broadband seismic stations and subsequently determine the fast orientation and the magnitude of crustal azimuthal anisotropy by fitting the sinusoidal moveout of the <fi>P</fi> to <fi>S</fi> converted phases from the Moho and intracrustal discontinuities. The magnitude of crustal anisotropy is found to range from 0.06 s to 0.54?s, with an average of 0.25 ± 0.08?s. Fault‐parallel anisotropy in the seismically active Zhangjiakou‐Penglai Fault Zone is significant and could be related to fluid‐filled fractures. Historical strong earthquakes mainly occurred in the fault zone segments with significant crustal anisotropy, suggesting that the measured crustal anisotropy is closely related to the degree of crustal deformation. The observed spatial distribution of crustal anisotropy suggests that the northwestern terminus of the fault zone probably ends at about 114°E. Also observed is a sharp contrast in the fast orientations between the western and eastern Yanshan Uplifts separated by the North‐South Gravity Lineament. The NW‐SE trending anisotropy in the western Yanshan Uplift is attributable to “fossil” crustal anisotropy due to lithospheric extension of the CNCC, while extensional fluid‐saturated microcracks induced by regional compressive stress are responsible for the observed ENE‐WSW trending anisotropy in the eastern Yanshan Uplift. Comparison of crustal anisotropy measurements and previously determined upper mantle anisotropy implies that the degree of crust‐mantle coupling in the CNCC varies spatially. </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”XML：ID =“GGGE21880-ABS-ABS-0001”> <标题类型=“main”>抽象</ title> > 为了在中央华北克拉顿（CNCC）下方的地壳各向异性，我们应用最近开发的去卷积方法，以有效地去除在200个宽带地震站的接收器功能中的近表面混响，随后确定出速取向和地壳方位角的大小通过拟合窦形扭转的各向异性 <fi> p </ fi> 到 <fi> s </ fi> 从Moho和颅内不连续转换阶段。发现地壳各向异性的大小范围为0.06秒至0.54°S，平均为0.25±0.08≤S。地震活跃的张家口 - 蓬莱断层区的断层平行各向异性是显着的，可能与流体填充的骨折有关。历史强大地震主要发生在具有显着的地壳各向异性的断层区段中，表明测量的地壳各向异性与地壳变形程度密切相关。观察到的地壳各向异性的空间分布表明故障区的西北末端可能在大约114°E中结束。在南北重力界面分开的西部和东部燕山隆起之间的快速取向也观察到的是一种鲜明对比。西燕山隆起的NW-SE趋势各向异性可归因于CNCC岩石局长的“化石”地壳各向异性，而区域压缩应力诱导的延伸流体饱和的微裂纹负责观察到的eNE-WSW趋势各向异性燕山东方隆起。地壳各向异性测量和先前确定的上部地幔各向异性的比较意味着CNCC中的外壳偶联程度在空间上变化。 </ 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>2019年第5期</span><b style="margin: 0 2px;">|</b><span>共17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=Zheng Tuo&option=202" target="_blank" rel="nofollow">Zheng Tuo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ding Zhifeng&option=202" target="_blank" rel="nofollow">Ding Zhifeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ning Jieyuan&option=202" target="_blank" rel="nofollow">Ning Jieyuan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Kelly H.&option=202" target="_blank" rel="nofollow">Liu Kelly H.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Stephen S.&option=202" target="_blank" rel="nofollow">Gao Stephen S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chang Lijun&option=202" target="_blank" rel="nofollow">Chang Lijun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Kong Fansheng&option=202" target="_blank" rel="nofollow">Kong Fansheng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fan Xiaoping&option=202" target="_blank" rel="nofollow">Fan Xiaoping;</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>Institute of GeophysicsChina Earthquake AdministrationBeijing China;</p> <p>Institute of GeophysicsChina Earthquake AdministrationBeijing China;</p> <p>School of Earth and Space SciencesPeking UniversityBeijing China;</p> <p>Geology and Geophysics ProgramMissouri University of Science and TechnologyRolla MO USA;</p> <p>Geology and Geophysics ProgramMissouri University of Science and TechnologyRolla MO USA;</p> <p>Institute of GeophysicsChina Earthquake AdministrationBeijing China;</p> <p>Geology and Geophysics ProgramMissouri University of Science and TechnologyRolla MO USA;</p> <p>College of Transportation Science and EngineeringNanjing Tech UniversityNanjing 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=seismic anisotropy&option=203" rel="nofollow">seismic anisotropy;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=North China Craton&option=203" rel="nofollow">North China Craton;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=receiver function&option=203" rel="nofollow">receiver function;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal deformation&option=203" rel="nofollow">crustal deformation;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yanshan Uplift&option=203" rel="nofollow">Yanshan Uplift;</a> </p> <div class="translation"> 机译：地震各向异性;华北克拉顿;接收器功能;地壳变形;燕山隆起; </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/0704023360828.html">Crustal Azimuthal Anisotropy Beneath the Central North China Craton Revealed by Receiver Functions</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zheng Tuo&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zheng Tuo,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ding Zhifeng&option=202" target="_blank" rel="nofollow" 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2013-05-01</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130443708051.html">System for influencing functions in a motor vehicle via a telematics device, has a transmitter/receiver unit in the vehicle and a remote mainframe/central processing unit with a receiver/transmitter</a> <b>[P]</b> . <span> 外国专利：  DE10141539A1 </span> <span> . 2003-03-13</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: break-all;white-space: initial;text-overflow: initial;overflow: initial;"> <span>机译：通过远程信息处理设备影响汽车功能的系统，具有车辆中的发送器/接收器单元和带有接收器/发送器的远程主机/中央处理单元 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130447396918.html">GPS RECEIVER WITH DR FUNCTION CAPABLE OF CORRECTING MEASUREMENT POSITION AND AZIMUTH</a> <b>[P]</b> . <span> 外国专利：  JP2002213979A </span> <span> . 2002-07-31</span> </div> <p class="zwjiyix translation" style="max-width: initial;height: auto;word-break: 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