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Final Assembly of the Southwestern Central Asian Orogenic Belt as Constrained by the Evolution of the South Tianshan Orogen: Links With Gondwana and Pangea

机译：由南天山oreoN的演变的南南部欧洲敌人皮带的最终组装：与Gondwana和Pangea的联系

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Abstract >The South Tianshan Orogen marks the final assembly of the southwestern Central Asian Orogenic Belt (CAOB) and the Karakum–Tarim cratons. Here we present an integrated mineralogical, geochemical, and geochronological study of the Wuwamen ophiolitic mélange in the South Tianshan to better understand the tectonic evolution of the western CAOB and its links to Gondwana and Pangea. Mantle peridotites with mineral compositions similar to those of abyssal peridotites and basalts with N‐MORB geochemical affinities suggest that the Wuwamen ophiolite was formed in a mid‐ocean ridge setting. Arc‐related gabbro and plagiogranite stocks intruding the mantle peridotites yielded zircon U–Pb ages of 441.1?±?4.2 and 442.8?±?2.4?Ma, indicating that the Wuwamen ophiolite got emplaced prior to ~440?Ma. Sericite‐quartz schist from the ophiolitic mélange matrix with abundant 481–319 Ma detrital zircon grains is crosscut by a two‐mica granite dike with a zircon U–Pb age of 321.3?±?1.7?Ma, thereby constraining the formation of the Wuwamen ophiolitic mélange at ~320?Ma. In conjunction with published data, we propose that the South Tianshan Ocean opened in the late Neoproterozoic and promoted the subsequent separation of microcontinents in the western CAOB from the northeast Gondwana margin during Gondwana assembly. Furthermore, the closure of the South Tianshan Ocean led to the final assembly of the southwestern CAOB and the Karakum–Tarim cratons and their incorporation into Pangea at ~320?Ma. </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> >南天山orgen标志着西南部中南造山带（曹）的最终组装卡拉库姆 - 塔里木克拉顿。在这里，我们展示了南天山武旺文化型眼镜的一体化矿物学，地球化学和地理学研究，以更好地了解西曹和鹅卵石的构造演变。与矿物质组合物的岩石偏见与矿物质组合物相似，类似于患有N-MORB地球化学亲色性亲子性的沼泽地表明，在海洋脊设定中形成了Wummen Ophiolite。与电弧相关的Gabbro和斑块岩石血液缺陷的岩石橄榄石产生441.1Ω·€α-±4.2和442.8？±2.4·mA，表明Wumen ophiolite在〜440〜440之前被施加。来自OphiolityMélange矩阵的Sericite-Quartz Schist具有丰富的481-319 mA碎屑锆石颗粒是双云母花岗岩堤的横切，锆石U-PB年龄为321.3Ω·€？1.7？1.7·马，从而限制了武瓦的形成OphioliticMélange在〜320？ma。与已发表的数据一起，我们建议南天山海洋在晚期开放，并在Gondwana集会期间促进了来自东北巩固山脉边缘的西曹中的微肠分离。此外，南天山海洋的关闭导致了西南曹家和卡拉库姆 - 塔里木克拉顿的最后装配及其在〜320〜320中的康艾结合。</ 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-34677/'>《Journal of geophysical research. Solid earth: JGR》</a> <b style="margin: 0 2px;">|</b><span>2018年第9期</span><b style="margin: 0 2px;">|</b><span>共28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=Wang Xin‐Shui&option=202" target="_blank" rel="nofollow">Wang Xin‐Shui;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klemd Reiner&option=202" target="_blank" rel="nofollow">Klemd Reiner;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Jun&option=202" target="_blank" rel="nofollow">Gao Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiang Tuo&option=202" target="_blank" rel="nofollow">Jiang Tuo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Ji‐Lei&option=202" target="_blank" rel="nofollow">Li Ji‐Lei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xue Sheng‐Chao&option=202" target="_blank" rel="nofollow">Xue Sheng‐Chao;</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 Mineral ResourcesInstitute of Geology and Geophysics Chinese Academy of SciencesBeijing China;</p> <p>GeoZentrum NordbayernUniversit?t Erlangen‐NürnbergErlangen Germany;</p> <p>Key Laboratory of Mineral ResourcesInstitute of Geology and Geophysics Chinese Academy of SciencesBeijing China;</p> <p>Laboratory of Isotope GeochemistryWuhan Centre of China Geological SurveyWuhan China;</p> <p>Key Laboratory of Mineral ResourcesInstitute of Geology and Geophysics Chinese Academy of SciencesBeijing China;</p> <p>State Key Laboratory of Geological Processes and Mineral ResourcesChina University of GeosciencesBeijing 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=Central Asian orogenic belt&option=203" rel="nofollow">Central Asian orogenic belt;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Tianshan&option=203" rel="nofollow">Tianshan;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wuwamen ophiolite&option=203" rel="nofollow">Wuwamen ophiolite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gondwana&option=203" rel="nofollow">Gondwana;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Pangea&option=203" rel="nofollow">Pangea;</a> </p> <div class="translation"> 机译：中亚造山带;天山;武旺根异丙石;GONDWANA;Pangea; </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/0704025592890.html">Final Assembly of the Southwestern Central Asian Orogenic Belt as Constrained by the Evolution of the South Tianshan Orogen: Links With Gondwana and Pangea</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wang Xin‐Shui&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Wang Xin‐Shui,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Klemd Reiner&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Klemd Reiner,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Gao Jun&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Gao Jun,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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