Moho Depth Variations From Receiver Function Imaging in the Northeastern North China Craton and Its Tectonic Implications

Zhang Ping; Yao Huajian; Chen Ling; Fang Lihua; Wu Yan; Feng Jikun

摘要

Abstract >A detailed knowledge of the crustal thickness in the northeastern North China Craton (NCC) is important for understanding the unusual Phanerozoic destruction of the craton. We achieve this goal by employing a 2‐D wave equation‐based migration method to P receiver functions from 198 broadband seismic stations, using Ps conversions and surface‐reflected multiples. By combining receiver function images along 19 profiles, we constructed a high‐resolution Moho depth model for the northeastern NCC. The results present dominant E‐W Moho depth variations similar to previous observations and new regional N‐S variations beneath both sides of the North‐South Gravity Lineament. To the west, while a deeper Moho (～42?km) appears in the interior of the Trans‐North China Orogen, a relatively shallow Moho (～38?km) exists in the northern margin of the Trans‐North China Orogen to western NCC. To the east, the crust beneath the Yan Mountains in the marginal area is thicker (～32–40?km) than that (～26–32?km) beneath the Bohai Bay Basin in the craton interior, and the Moho further shallows from NE (～32?km) to SW (～26?km) within the basin. Along with other observations, we conclude that the dominant E‐W difference may have been associated with the Paleo‐Pacific plate subduction under eastern Asia since the Mesozoic. The newly observed complex N‐S variations may have reflected the structural heterogeneity of the cratonic lithosphere inherited since the formation of the NCC in the Paleoproterozoic, or spatially uneven effects on the cratonic lithosphere of subsequent thermotectonic events during the long‐term evolution of the craton, or both. </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 =“JGRB53290-ABS-ABS-ABS-0001”> <标题类型=“MAIN”> Abstract </ Title> <P>详细知识的地壳厚度东北地球克拉顿（NCC）对理解克拉顿的不寻常的挑战是重要的。我们通过使用PS转换和表面反射倍数采用来自198个宽带地震站的P接收器功能来实现这一目标。通过沿着19个配置文件组合接收器函数图像，我们为NCC东北部建造了一个高分辨率的Moho深度模型。结果存在主导的E-W Moho深度变化，类似于先前的观察和北方重力线的两侧下方的新区域N-S变化。在西方，虽然更深层次的Moho（〜42 km）出现在跨北oreoN的内部，但在Trans-North China Orogen oregane到西方的北部边缘存在相对较浅的Moho（〜38 km） NCC。到东方，边缘地区燕山下的地壳比渤海湾盆地在堡垒内部（〜26-32 km）厚度（〜32-40 km），而Moho进一步浅Ne（〜32 km）到盆内的SW（〜26 km）。随着其他观察结果，我们得出结论，由于中生代以来，主导E-W差异可能与东亚的古太平洋板介绍有关。新观察到的复合N-S变化可能反映了克拉汀岩石圈的结构异质性，因为在古典古古代的NCC形成的NCC或对克拉顿的长期演进期间随后的热电偶事件的克拉氏岩石圈的空间不均匀的影响，或两者。</ 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>2019年第2期</span><b style="margin: 0 2px;">|</b><span>共19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 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=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=Chen Ling&option=202" target="_blank" rel="nofollow">Chen Ling;</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> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Yan&option=202" target="_blank" rel="nofollow">Wu Yan;</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> </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>Institute of Geology and GeophysicsChinese Academy of SciencesBeijing China;</p> <p>Institute of GeophysicsChina Earthquake AdministrationBeijing China;</p> <p>Institute of GeophysicsChina Earthquake AdministrationBeijing 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> </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=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=Moho depth&option=203" rel="nofollow">Moho depth;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=receiver function imaging&option=203" rel="nofollow">receiver function imaging;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithospheric destruction&option=203" rel="nofollow">lithospheric destruction;</a> </p> <div class="translation"> 机译：华北克拉顿;Moho深度;接收器功能成像;岩石树形破坏; </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/0704025592328.html">Moho Depth Variations From Receiver Function Imaging in the Northeastern North China Craton and Its Tectonic Implications</a> <b>[J]</b> . <span> <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" class="tuijian_auth tuijian_authcolor">Zhang Ping,</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=Chen Ling&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chen Ling,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Ikuo Katayama,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tomoeki Nakakuki&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Tomoeki Nakakuki </a> <span>-1</span> </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：莫霍面流变解耦及其对金星构造的启示</span> </p> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/open-access_resources_thesis/01000129021456.html">Erratum: Lithospheric structure beneath the central and western North China Craton and adjacent regions from S-receiver function imaging</a> <b>[O] </b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yaoyang Zhang&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yaoyang Zhang,</a> <a 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J.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Michael, P. J.,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Bonatti, E.&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Bonatti, E. </a> <span>1985</span> </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：来自北大西洋的橄榄岩组成：区域和构造变化及其对部分熔融的影响</span> </p> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/academic-journal-cn_chinese-journal-geophysics_thesis/0201278804664.html">远震接收函数确定的鄂尔多斯西部及邻区Moho面性质和构造意义</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=黄柳婷&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 黄柳婷</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=沈旭章&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,沈旭章</a> <a 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