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Seismic Evidence for a Mantle Transition Zone Origin of the Wudalianchi and Halaha Volcanoes in Northeast China

机译：中国东北地区华美和哈拉哈火山的地幔过渡区的地震证据

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Abstract > There exists much debate about origins of Cretaceous to present volcanism in northeast (NE) China. Here we present high‐resolution seismic images of the upper mantle beneath NE China obtained by inverting P wave traveltime data recorded by two dense linear arrays. The inclusion of the new data set has greatly improved sampling of the upper mantle beneath the study region, providing tight constraints on the seismic structure under the intraplate Wudalianchi and Halaha volcanoes. Local‐scale low P wave velocity (low‐Vp) anomalies are revealed in the shallow mantle beneath the two volcanoes, whereas a large‐scale high‐Vp zone is imaged in the mantle transition zone. These new results suggest that the two volcanoes, though located at different sites above the stagnant Pacific slab in the mantle transition zone, are likely related to the deep subduction and dehydration of the Pacific slab, possibly through hot and wet upwelling in the big mantle wedge beneath Wudalianchi and through deeper hydrous upwelling related to slab avalanche beneath Halaha. Our results also reveal other striking features, such as high‐Vp anomalies resting atop the 410‐km discontinuity beneath the Great Xing'an Range and the Songliao Basin, which are attributed to detached continental lithosphere. The delamination most likely occurred in the Cretaceous, which induced widespread magmatism in NE China. </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> > 关于在东北（NE）中国的白垩纪起源的起源存在很多争论。在这里，我们目前通过反转获得的NE中国下部地幔的高分辨率地震图像 p </ i> 波旅行时间数据由两个密集的线性阵列记录。包含新的数据集在研究区域下面的上部地幔的采样大大提高，为intraLate Wudianchi和Halaha火山下的地震结构提供了严格的限制。局部规模低 p </ i> 波速（低VP）异常在两个火山下方的浅地幔中透露，而大规模的高VP区在披风过渡区中成像。这些新结果表明，两座火山虽然位于地幔过渡带的滞留太平洋板块上方的不同部位，但可能与太平洋平板的深俯冲和脱水有关，可能通过大型地幔楔形的热和湿润的上升沃达利亚奇下面，通过哈拉哈下面的平板雪崩相关的深层潮湿。我们的结果还揭示了其他引人注目的功能，例如高兴安范围和松辽盆地的410公里处的高VP异常休息，归因于独立式大陆岩石圈。分层最有可能发生在白垩纪，诱导在中国的广泛岩浆广告。 </ 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1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=Wei Wei&option=202" target="_blank" rel="nofollow">Wei Wei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hammond James O. S.&option=202" target="_blank" rel="nofollow">Hammond James O. S.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhao Dapeng&option=202" target="_blank" rel="nofollow">Zhao Dapeng;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Jiandong&option=202" target="_blank" rel="nofollow">Xu Jiandong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Qian&option=202" target="_blank" rel="nofollow">Liu Qian;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gu Yaning&option=202" target="_blank" rel="nofollow">Gu Yaning;</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>Key Laboratory of Active Tectonics and Volcano Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>Department of Earth and Planetary Sciences BirkbeckUniversity of LondonLondon UK;</p> <p>Department of Geophysics Graduate School of ScienceTohoku UniversitySendai Japan;</p> <p>Key Laboratory of Active Tectonics and Volcano Institute of GeologyChina Earthquake AdministrationBeijing China;</p> <p>Beijing Applied Meteorology InstituteBeijing China;</p> <p>Key Laboratory of Active Tectonics and Volcano Institute of GeologyChina 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=seismic tomography&option=203" rel="nofollow">seismic tomography;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wudalianchi volcano&option=203" rel="nofollow">Wudalianchi volcano;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Halaha volcano&option=203" rel="nofollow">Halaha volcano;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pacific slab&option=203" rel="nofollow">Pacific slab;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=mantle transition zone&option=203" rel="nofollow">mantle transition zone;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lithospheric delamination&option=203" rel="nofollow">lithospheric delamination;</a> </p> <div class="translation"> 机译：地震层析成像;乌维提Chlcano;Halaha Volcano;太平洋板块;地幔过渡区;岩石层分层; </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/0704023360434.html">Seismic Evidence for a Mantle Transition Zone Origin of the Wudalianchi and Halaha Volcanoes in Northeast China</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wei Wei&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wei Wei,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hammond James O. 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