Linear Array Ambient Noise Adjoint Tomography Reveals Intense Crust‐Mantle Interactions in North China Craton

机译：线性阵列环境噪声伴随断层扫描揭示了华北克拉顿的激烈的地壳互动

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Abstract >We present a 2‐D ambient noise adjoint tomography technique for a linear array with a significant reduction in computational cost and show its application to an array in North China. We first convert the observed data for 3‐D media, i.e., surface‐wave empirical Green's functions (EGFs) to the reconstructed EGFs (REGFs) for 2‐D media using a 3‐D/2‐D transformation scheme. Different from the conventional steps of measuring phase dispersion, this technology refines 2‐D shear wave speeds along the profile directly from REGFs. With an initial model based on traditional ambient noise tomography, adjoint tomography updates the model by minimizing the frequency‐dependent Rayleigh wave traveltime delays between the REGFs and synthetic Green functions calculated by the spectral‐element method. The multitaper traveltime difference measurement is applied in four‐period bands: 20–35?s, 15–30?s, 10–20?s, and 6–15?s. The recovered model shows detailed crustal structures including pronounced low‐velocity anomalies in the lower crust and a gradual crust‐mantle transition zone beneath the northern Trans‐North China Orogen, which suggest the possible intense thermo‐chemical interactions between mantle‐derived upwelling melts and the lower crust, probably associated with the magmatic underplating during the Mesozoic to Cenozoic evolution of this region. To our knowledge, it is the first time that ambient noise adjoint tomography is implemented for a 2‐D medium. Compared with the intensive computational cost and storage requirement of 3‐D adjoint tomography, this method offers a computationally efficient and inexpensive alternative to imaging fine‐scale crustal structures beneath linear arrays. </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> >我们为线性阵列提供了一个二维环境噪声伴随断层扫描技术，具有显着减少在计算成本中，将其应用于华北地区的阵列。我们首先使用3-D / 2-D转换方案将观察到的3-D媒体，即表面波经验绿色的功能（EGFS）转换为2-D介质的重建EGFS（EGF）。与测量相色散的传统步骤不同，该技术直接从Regfs沿着轮廓精确沿轮廓的2-D剪切波速。利用基于传统环境噪声断层扫描的初始模型，通过最小化通过光谱元件方法计算的Regfs和合成绿色函数之间的频率相关的瑞利波行程延迟来更新模型。多销旅行时间差测量应用于四个周期带：20-35？S，15-30？S，10-20？S和6-15秒。恢复的模型显示了详细的地壳结构，包括下地壳中的明显低速异常和北部跨国北部奥根根下方的渐进的地壳 - 地幔过渡区，这表明了地幔衍生的上升融化之间可能的强烈热化学相互作用下地壳，可能与在中生代到该区域的新生代演变期间的岩石底层相关。据我们所知，它是第一次为2-D培养基实施环境噪声伴随断层扫描。与3-D伴随断层扫描的密集计算成本和存储需求相比，该方法提供了在线性阵列下的成像微尺度地壳结构的计算有效和廉价的替代方案。</ 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>2018年第1期</span><b style="margin: 0 2px;">|</b><span>共16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=Zhang Chao&option=202" target="_blank" rel="nofollow">Zhang Chao;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Huajian&option=202" target="_blank" rel="nofollow">Yao Huajian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Qinya&option=202" target="_blank" rel="nofollow">Liu Qinya;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Ping&option=202" target="_blank" rel="nofollow">Zhang Ping;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yuan Yanhua O.&option=202" target="_blank" rel="nofollow">Yuan Yanhua O.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Feng Jikun&option=202" target="_blank" rel="nofollow">Feng Jikun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Fang Lihua&option=202" target="_blank" rel="nofollow">Fang Lihua;</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>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Department of PhysicsUniversity of TorontoToronto Ontario Canada;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Department of GeosciencesPrinceton UniversityPrinceton NJ USA;</p> <p>Laboratory of Seismology and Physics of Earth's Interior School of Earth and Space SciencesUniversity of Science and Technology of ChinaHefei China;</p> <p>Institute of GeophysicsChina Earthquake AdministrationBeijing 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=adjoint tomography&option=203" rel="nofollow">adjoint tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=ambient noise&option=203" rel="nofollow">ambient noise;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=surface waves&option=203" rel="nofollow">surface waves;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=3‐D/2‐D transformation&option=203" rel="nofollow">3‐D/2‐D transformation;</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=crustal structure&option=203" rel="nofollow">crustal structure;</a> </p> <div class="translation"> 机译：伴随断层扫描;环境噪声;表面波;3-D / 2-D转换;华北;地壳结构; </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/0704025592818.html">Linear Array Ambient Noise Adjoint Tomography Reveals Intense Crust‐Mantle Interactions in North China Craton</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Chao&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Zhang Chao,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yao Huajian&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yao Huajian,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Qinya&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Liu Qinya,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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