The Role of Recycled Oceanic Crust in the Generation of Alkaline A‐Type Granites

机译：再生海外壳在碱性A型花岗岩中的作用

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Abstract > Melting and dehydration of subducted oceanic slabs dominate element recycling within the subduction factory, but the role of recycled oceanic crust in the source of intraplate magmas is poorly understood. In situ zircon O‐Hf isotope data from two Early Cretaceous alkaline A‐type granites that are genetically related to large‐scale extension of eastern China in the Late Mesozoic (circa 125 Ma) yield low δ 18 O (1.8?±?0.3‰ to 5.1?±?0.3‰, 2 <fi>σ</fi> ) and positive εHf( <fi>t</fi> ) (1.5?±?1.2 to 17?±?1.2, 2 <fi>σ</fi> ). This suggests the contribution of altered oceanic crust and an enriched mantle component in the source region. Elevated initial 87 Sr/ 86 Sr and 206 Pb/ 204 Pb ratios, and εHf( <fi>t</fi> ) whole rock values with relatively constant εNd( <fi>t</fi> ) values beyond the normal mantle array, require a component that underwent seawater interaction in the source of protolith. The geochemical data require a complex source region for the alkaline A‐type granites in NE China involving more than 40% recycled oceanic crust. This altered oceanic crust beneath the Late Mesozoic lithospheric mantle likely represents remnants of multiple subduction and collision events between microblocks from the Late Paleozoic to Early Mesozoic in northeastern China. Recycling of subducted oceanic crust represents a novel exotic source for the origin of alkaline A‐type granites in intraplate extensional settings. </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”>摘要</ title> >后果海洋板块的熔化和脱水在俯冲厂内的元素回收的核对元素回收在陷阱岩石源的回收海洋地壳被理解得很差。原位锆石O-HF同位素数据来自两种早期白垩纪碱性A型花岗岩，遗传有关中西代的晚期大规模的大规模延伸（大约125 mA）产量低δ 18 </ sup> o （1.8？±0.3°至5.1°±0.3°，2 <fi>σ</ fi>）和正εhf（<fi> t </ fi>）（1.5？±1.2至17？±1.2 ，2 <fi>σ</ fi>）。这表明源区中改变的海壳和富含富含的地幔组分的贡献。升高的初始 87 </ sup> sr / 86 </ sup> sr和 206 </ sup> pb / 204 </ sup> pb比率，εhf（<fi> t </ fi>）具有相对恒定的εnd（<fi> t </ fi>）值的整个岩石值，超出正常的地幔阵列，需要在促果子源中进行海水相互作用的组件。地球化学数据需要在纳米中国碱性A型花岗岩需要复杂的源区，涉及超过40％的循环的海壳。这种改变的海洋外壳下方的后期型岩石地幔可能代表来自中国东北部早期古生代古生代古群的微块之间的多个胶片和碰撞事件的残余。底层海底的再循环代表了血管内部扩展设置中碱性A型花岗岩起源的新型异乎寻常的源。 </ 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>2017年第12期</span><b style="margin: 0 2px;">|</b><span>共9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=Yang Wu‐Bin&option=202" target="_blank" rel="nofollow">Yang Wu‐Bin;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niu He‐Cai&option=202" target="_blank" rel="nofollow">Niu He‐Cai;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hollings Pete&option=202" target="_blank" rel="nofollow">Hollings Pete;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zurevinski Shannon E.&option=202" target="_blank" rel="nofollow">Zurevinski Shannon E.;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Li Ning‐Bo&option=202" target="_blank" rel="nofollow">Li Ning‐Bo;</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 Mineralogy and Metallogeny Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Key Laboratory of Mineralogy and Metallogeny Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>Department of GeologyLakehead UniversityThunder Bay Ontario Canada;</p> <p>Department of GeologyLakehead UniversityThunder Bay Ontario Canada;</p> <p>Key Laboratory of Mineralogy and Metallogeny Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou 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=Recycled oceanic crust&option=203" rel="nofollow">Recycled oceanic crust;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=A‐type granite&option=203" rel="nofollow">A‐type granite;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zircon O‐Hf isotopes&option=203" rel="nofollow">Zircon O‐Hf isotopes;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Low δ18O magma&option=203" rel="nofollow">Low δ18O magma;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=NE China&option=203" rel="nofollow">NE China;</a> </p> <div class="translation"> 机译：再生海外壳;一种型花岗岩;锆石O-HF同位素;低δ18O岩浆;NE中国; </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/0704025592773.html">The Role of Recycled Oceanic Crust in the Generation of Alkaline A‐Type Granites</a> <b>[J]</b> . <span> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Yang Wu‐Bin&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Yang Wu‐Bin,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Niu He‐Cai&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Niu He‐Cai,</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Hollings Pete&option=202" target="_blank" rel="nofollow" class="tuijian_auth tuijian_authcolor">Hollings Pete,</a> <a href="/journal-foreign-34677/" target="_blank" rel="nofollow" class="tuijian_authcolor">Journal of geophysical research. 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