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Melt‐Fluxed Melting of the Heterogeneously Mixed Lower Arc Crust: A Case Study from the Qinling Orogenic Belt, Central China

机译：异质混合下弧外壳的熔融熔融：中部秦岭造山带的案例研究

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Abstract > Adakitic rocks with high MgO content and lower crust affinity at convergent margins provide important constraints on arc crust evolution and regional tectonics. An integrated study on the only adakitic pluton with high MgO content and its mafic microgranular enclaves (MMEs) in the Early Paleozoic North Qinling arc terrane was conducted in this paper. Zircons from 2 host rock samples yielded identical weighted mean ages of 428 Ma. The MMEs contain two types of zircons: type 1 zircons share similar morphology, chemical composition, and indistinguishable age with those from the host rock; type 2 zircons yielded an older age of 450 Ma. The similarity in zircon Hf isotopic composition for these zircons indicates a cognate origin of the MMEs. However, the lower Ce 4+ /Ce 3+ , higher crystallization temperature and the LREE overabundance of type 2 zircons indicate that mafic intrusions in the lower arc crust were subjected to a post‐magmatic event at ～450 Ma. Samples from the Tangzang pluton are characterized by typical adakitic geochemical features, and high MgO (Mg # : 50–52), Cr, Ni, and Ba contents. Considering their similar isotopic compositions with the Neoproterozoic metabasites in the North Qinling terrane, we argue that the Tangzang pluton was generated by crustal anatexis of two sources with contributions from the metasomatized mantle wedge. The mantle connection was achieved by aqueous melt‐fluxed melting of a “hot zone” in the lower arc crust. This implies that andesitic continental crust with Mg# of ～0.5 may also be associated with fluxed‐melting of the lower arc crust. </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”> <标题类型=“main”>抽象</ title> > 在收敛边缘的MgO含量和较低的地壳亲和力下具有高MgO含量和较低的地壳亲和力为弧性地壳进化和区域构造提供了重要的限制。本文在古生代北秦岭弧地区唯一具有高MgO含量及其迈克斯微血管飞地（MMES）唯一的储型芦苇的综合研究。来自2个宿主岩石样品的锆石产生相同的加权平均年龄428 mA。 MME含有两种类型的锆石：1型锆石与来自主体岩石的人共享相似的形态，化学成分和难以区分的年龄; 2型锆石越大，450 mA历史。这些锆石的锆石HF同位素组合物的相似性表明了MME的同源来源。但是，下层 4 + </ sup> / ce. 3 + </ sup> ，较高的结晶温度和2型锆菌的淋病过多表明，在〜450mA的后弧形外壳中的MAFIC入侵进行了后岩石事件。来自唐塘勘方的样品的特征在于典型的Adakitic地球化学特征和高MgO（Mg ＃</ sup> ：50-52），Cr，Ni和BA内容。考虑到与北秦岭地区的新蛋白质古代代表相似的同位素组成，我们认为唐塘芦苇由两个来源的地壳Anatexis产生，其中两个来源具有来自弥扑地幔楔的贡献。通过在下弧外壳中的“热区”的水性熔融熔融熔化来实现地幔连接。这意味着具有Mg＃的〜0.5的烯型大陆地壳也可以与下弧外壳的熔融熔化有关。 </ 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>2018年第6期</span><b style="margin: 0 2px;">|</b><span>共22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=Wu Kai&option=202" target="_blank" rel="nofollow">Wu Kai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ling Ming‐Xing&option=202" target="_blank" rel="nofollow">Ling Ming‐Xing;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hu Yong‐Bin&option=202" target="_blank" rel="nofollow">Hu Yong‐Bin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Guo Jia&option=202" target="_blank" rel="nofollow">Guo Jia;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Jiang Xiao‐Yan&option=202" target="_blank" rel="nofollow">Jiang Xiao‐Yan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Sai‐Jun&option=202" target="_blank" rel="nofollow">Sun Sai‐Jun;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liang Hua‐Ying&option=202" target="_blank" rel="nofollow">Liang Hua‐Ying;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Liu Xu&option=202" target="_blank" rel="nofollow">Liu Xu;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Sun Weidong&option=202" target="_blank" rel="nofollow">Sun Weidong;</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>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>CAS Key Laboratory of Mineralogy and MetallogenyGuangzhou Institute of Geochemistry Chinese Academy of SciencesGuangzhou China;</p> <p>211 Geological Team Sino Shaanxi Nuclear Industry GroupXi'an China;</p> <p>University of Chinese Academy of SciencesBeijing 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=the Tangzang pluton&option=203" rel="nofollow">the Tangzang pluton;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=adakitic rocks&option=203" rel="nofollow">adakitic rocks;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=lower arc crust&option=203" rel="nofollow">lower arc crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Qinling orogenic belt&option=203" rel="nofollow">Qinling orogenic belt;</a> </p> <div class="translation"> 机译：Tangzang芦苇;Adakitic岩石;下弧外壳;秦岭造山带; </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/0704023360440.html">Melt‐Fluxed Melting of the Heterogeneously Mixed Lower Arc Crust: A Case Study from the Qinling 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href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=瞿金平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,瞿金平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=刘跃军&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,刘跃军</a> <span> <a href="/journal-cn-9151/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 化工学报 </a> </span> <span> . 2009</span><span>,第003期</span> </span> </div> </li> <li> <div> <b>5. </b><a class="enjiyixqcontent" href="/academic-journal-cn_detail_thesis/0201292949418.html">岩石部分熔融过程中熔体连通性的实验研究——以850～1100 ℃,2.0～4.0 GPa条件下斜长角闪岩部分熔融为例</a> <b>[J]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑小刚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郑小刚</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李和平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李和平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周文戈&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周文戈</a> <span> <a href="/journal-cn-57400/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 矿物岩石地球化学通报 </a> </span> <span> . 2007</span><span>,第z1期</span> </span> </div> </li> <li> <div> <b>6. </b><a class="enjiyixqcontent" href="/academic-conference-cn_meeting-20295_thesis/0202269793.html">岩石部分熔融过程中熔体连通性的实验研究——以850～1100 ℃,2.0～4.0 GPa条件下斜长角闪岩部分熔融为例</a> <b>[C]</b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郑小刚&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郑小刚</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=李和平&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,李和平</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=周文戈&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">,周文戈</a> <span> <a href="/conference-cn-20295/" target="_blank" rel="nofollow" class="tuijian_authcolor"> . 中国矿物岩石地球化学学会第11届学术年会 </a> <span> <span> . 2007</span> </span> </div> </li> <li> <div> <b>7. </b><a class="enjiyixqcontent" href="/academic-degree-domestic_mphd_thesis/020312019841.html">氩弧熔融制备金刚石/铝复合材料的研究</a> <b>[A] </b> <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=郭冠华&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor"> . 郭冠华</a> <span> . 2017</span> </span> </div> </li> </ul> <ul style="display: none;"> <li> <div> <b>1. </b><a class="enjiyixqcontent" href="/patent-detail/061202245510.html">金属陶瓷熔射粉末、熔融金属镀浴用辊和熔融金属镀浴中部件</a> <b>[P]</b> . <span> 中国专利： CN104854253B </span> <span> . 2016.10.26</span> </div> </li> <li> <div> <b>2. </b><a class="enjiyixqcontent" href="/patent-detail/06120107342170.html">金属陶瓷熔射粉末、熔融金属镀浴用辊和熔融金属镀浴中部件</a> <b>[P]</b> . <span> 中国专利： CN104854253A </span> <span> . 2015-08-19</span> </div> </li> <li> <div> <b>3. </b><a class="enjiyixqcontent" href="/patent-detail/06130472961281.html">Procedure and device for melting of mixed flux material in an electric arc furnace</a> <b>[P]</b> . <span> 外国专利：  SE440438B </span> <span> . 1985-07-29</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：在电弧炉中熔化混合助熔剂材料的方法和装置 </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('0704023360440','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" 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