Lithospheric Structure of the Northern Ordos From Ambient Noise and Teleseismic Surface Wave Tomography

Li Shilin; Guo Zhen; Chen Yongshun John; Yang Yingjie; Huang Qinghua

摘要

Abstract > We constructed a high‐resolution 3‐D V <sub> s </sub> model of the northern Ordos block and its surrounding areas by surface wave tomography, which reveals significant intracratonic heterogeneities. In the western Ordos, the lithosphere thickness is ~200?km with shear velocities comparable to the high velocities of other Archean cratons worldwide. However, the lithosphere thins gradually toward the east and V <sub> s </sub> drops by 2–3% in the uppermost mantle beneath the eastern Ordos, coincident with the high surface heat flow (~68?mW/m 2 in average) there. This observation suggests that the thick, cratonic keel is only locally preserved beneath the western Ordos, and the eastern part of the Ordos seems to undergo local rejuvenation. At greater depths (>180?km), a low‐velocity channel is observed beneath the high‐velocity keel of the Ordos. Beneath the Datong volcanoes, a low‐velocity anomaly is observed, dipping westward with depth and closely following the slope of the lithosphere beneath the northern Ordos. This prominent low velocity is connected with the low‐velocity zone beneath the northern Ordos, which is further connected with the low‐velocity zone beneath the northeastern Tibetan Plateau (NET). We propose that the asthenosphere beneath the NET flows toward the northern Ordos in response to the continuous northward convergence of the Indian‐Eurasian continents, and the asthenosphere flows upward following the eastward thinning lithosphere which leads to decompression partial melting, which migrates upward to feed the Datong volcanoes. The significant variations of the lithospheric thickness of the Ordos block may control the distribution of the asthenospheric flow. </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”> <标题类型=“main”>抽象</ title> >我们构建了高分辨率3-D v </ i> <sub > S </ se>北部ORDOS块的模型及其表面波断层扫描的周围地区，揭示了显着的腹腔内异质性。在西部鄂尔多斯，岩石圈厚度为〜200 km，剪切速度与全球其他成员克拉顿的高速相当。然而，岩石圈逐渐向东逐渐朝向东部， v </ i> <sub> s 在东部鄂尔多斯的最上面的地幔中滴加2-3％，与在那里，高表面热流（〜68Ωmw/ m 2 </ sup>）。该观察表明，厚度，克拉密龙骨仅在西部鄂尔多斯下方被局存，鄂尔多斯的东部似乎正在接受本地的复兴。在更大的深度（> 180 km）时，在鄂尔多斯的高速龙骨下方观察到低速通道。在大同火山下方，观察到低速异常，深入倾向于北部鄂尔多斯下层岩石圈的斜坡。这种突出的低速与北鄂尔多斯下方的低速区连接，该低速区与东北藏高原（NET）下方的低速区相连。我们建议在净北部的北方鄂尔多斯下面的近年繁殖的哮喘圈，并且在向东稀薄的岩石圈后，哮喘圈向上流动，导致减压部分熔化，向上迁移以喂养大同火山。 ORDOS块的岩石晶体厚度的显着变化可以控制哮喘流动的分布。 </ 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=Li Shilin&option=202" target="_blank" rel="nofollow">Li Shilin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guo Zhen&option=202" target="_blank" rel="nofollow">Guo Zhen;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Yongshun John&option=202" target="_blank" rel="nofollow">Chen Yongshun John;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Yingjie&option=202" target="_blank" rel="nofollow">Yang Yingjie;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Huang Qinghua&option=202" target="_blank" rel="nofollow">Huang Qinghua;</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>Department of Ocean Science and EngineeringSouthern University of Science and TechnologyShenzhen China;</p> <p>Department of Ocean Science and EngineeringSouthern University of Science and TechnologyShenzhen China;</p> <p>Department of Ocean Science and EngineeringSouthern University of Science and TechnologyShenzhen China;</p> <p>CCFS GEMOC ARC National Key Centre Department of Earth and Planetary SciencesMacquarie UniversitySydney New South Wales Australia;</p> <p>Institute of Theoretical and Applied Geophysics School of Earth and Space SciencesPeking UniversityBeijing 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=craton destruction&option=203" rel="nofollow">craton destruction;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle flow&option=203" rel="nofollow">mantle flow;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=intraplate volcanism&option=203" rel="nofollow">intraplate volcanism;</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=Datong volcanoes&option=203" rel="nofollow">Datong volcanoes;</a> </p> <div class="translation"> 机译：Craton毁灭;地幔流;血液岩石主义;华北克拉顿;大同火山; </div> </li> </ul> </div> </div> <div class="literature cardcommon" id="literaturereference" style="display:none"> <div class="similarity "> <h3 class="all_title" id="enpatent111">引文网络</h3> <div class="referencetab clearfix"> <ul id="referencedaohang"> <li dataid="referenceul">参考文献</li> <li dataid="citationul">引证文献</li> <li dataid="commonreferenceul">共引文献</li> <li dataid="commoncitationul">同被引文献</li> <li dataid="tworeferenceul">二级参考文献</li> <li dataid="twocitationul">二级引证文献</li> </ul> </div> <div class="reference_details" id="referenceList"> <ul id="referenceul"></ul> <ul id="citationul"></ul> <ul id="commonreferenceul"></ul> <ul id="commoncitationul"></ul> <ul id="tworeferenceul"></ul> <ul id="twocitationul"></ul> </div> </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="/academic-journal-cn_journal-seismology-english-edition_thesis/0201252698151.html">Segmentations of active normal dip-slip faults around Ordos block accordingto their surface ruptures in historical strong earthquakes</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> </a> <a href="/journal-foreign-4884/" target="_blank" rel="nofollow" class="tuijian_authcolor">地震学报（英文版） .</a> <span>2000</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/journal-foreign-detail/0704025591040.html">Lithospheric Structure of the Northern Ordos From Ambient Noise and Teleseismic Surface Wave Tomography</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Shilin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Li Shilin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guo Zhen&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Guo Zhen,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Chen Yongshun John&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Chen Yongshun John,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑超</a> <span> <a href="/journal-cn-4795/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 岩石学报 </a> </span> <span> . 2009</span><span>,第010期</span> </span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/academic-journal-cn_journal-chengdu-university-technology-science-technology-edition_thesis/0201248799907.html">川东北下三叠统飞仙关组白云岩成因——来自岩石结构的证据</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=高梅生&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 高梅生</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑荣才&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑荣才</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=文华国&option=202" target="_blank" rel="nofollow" class="tuijian_auth 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2020</span><span>,第005期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-20238_thesis/0202255243.html">川东北地区飞仙关组白云岩成因研究-来自岩石结构、微量元素和Sr同位素的证据</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑荣才&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郑荣才</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李国军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李国军</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑超&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,郑超</a> <span> <a href="/conference-cn-20238/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 2007年油气藏地质及开发工程国家重点实验室第四次国际学术会议 </a> <span> <span> . 2007</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/02031114299.html">南海北部海域环境噪声空间相关特性研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李羽弘&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 李羽弘</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061203857207.html">南海北部内孤立波的预测方法及系统</a> <b>[P]</b> . <span> 中国专利： CN110285944B </span> <span> . 2020.07.28</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120101166770.html">南海北部内孤立波的预测方法及系统</a> <b>[P]</b> . <span> 中国专利： CN110285944A </span> <span> . 2019-09-27</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130401868511.html">Internal wave ambient noise tomography for antisubmarine warfare</a> <b>[P]</b> . <span> 外国专利：  US10634765B1 </span> <span> . 2020-04-28</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：内波环境噪声层析成像技术在反潜战中的应用 </span> </p> </li> <li> <div> <b>4. </b><a class="enjiyixqcontent" href="/patent-detail/06130424528693.html">ULTRASONIC WAVE SENSOR FIXING STRUCTURE FOR REDUCING SIGNAL NOISE RATIO BY CONTROLLING A SURFACE WAVE AND AN ULTRASONIC SENSOR MOUNTING PLATFORM USING THE SAME</a> <b>[P]</b> . <span> 外国专利：  KR20110090514A </span> <span> . 2011-08-10</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：超声波传感器固定结构，通过使用相同的方法控制表面波和超声波传感器安装平台来降低信号噪声比 </span> </p> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/patent-detail/06130424315903.html">Electrical device i.e. electronic computer system, has housing for accommodating electrical components e.g. capacitors and resistors, and generating sound source ambient noise, and acoustic cavity resonator for damping sound waves</a> <b>[P]</b> . <span> 外国专利：  DE102009037417A1 </span> <span> . 2011-02-17</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：电气设备，即电子计算机系统，具有用于容纳电气部件的外壳，例如电容器和电阻器，产生声源环境噪声，以及用于衰减声波的声腔谐振器 </span> </p> </li> </ul> </div> </div> </div> <div class="theme cardcommon" style="overflow: auto;display:none"> <h3 class="all_title" id="enpatent55">相关主题</h3> <ul id="subject"> </ul> </div> </div> </div> </div> <div class="right rightcon"> <div class="details_img cardcommon clearfix" style="margin-bottom: 10px;display:none;" > </div> </div> </div> <div id="thesis_get_original1" class="downloadBth" style="bottom: 19px;z-index: 999;" onclick="ywcd('0704025591040','4',7,2,1,'',this,24)" class="delivery" prompt="010401" title="通过人工服务将文献原文发送至邮箱" >获取原文</div> <div class="journalsub-pop-up" 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