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Petrological and Geochemical Constraints on the Origin of Early Cretaceous Volcanic Rocks in the Central‐East Asia: Implications for Crustal Growth and Evolution

机译：中东亚洲早期白垩纪火山岩起源的岩石和地球化学约束：地壳增长和进化的影响

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Abstract > New petrological and geochemical data for Early Cretaceous volcanic rocks in the North China Craton (NCC) combined with published data of cotemporaneous volcanic rocks in the NCC and eastern Central Asian Orogenic Belt (ECAOB) are used to understand their petrogenesis and crustal growth and evolution. Early Cretaceous volcanic rocks in the NCC show characteristics typical of continental crust, with negative Nb and Ta anomalies, and enrichment of K and Pb. The εNd of Early Cretaceous volcanic rocks in the NCC correlate with indices of differentiation (e.g., Mg#), implying that mantle‐derived magmas were modified by open‐system processes. The high‐Mg clinopyroxene and melt inclusions hosted by high‐Fo olivine in Early Cretaceous volcanic rocks in the NCC have lower 207 Pb/ 206 Pb and 208 Pb/ 206 Pb ratios than low‐Mg clinopyroxene and melt inclusions hosted by low‐Fo olivine, which can be explained by the interaction between lower crust and basaltic magmas (magma mixing or assimilation). Unlike contemporaneous counterparts in the NCC, Early Cretaceous volcanic rocks in the ECAOB have high εNd values. Such features can also be produced by crustal assimilation and/or magma mixing, given the juvenile lower crust beneath the ECAOB. The “adakitic” signature of Early Cretaceous volcanic rocks is most likely inherited from the lower continental crust. Large‐scale partial melting of the lower crust may have been related to continuous magmatic underplating in an extensional environment. This work suggests that Early Cretaceous volcanic rocks in the Central‐East Asia represent a nonnegligible contribution to crustal growth, despite having “crust‐like” trace element and isotopic characteristics. </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> > 华北CRATON（NCC）早期白垩纪火山岩的新岩石和地球化学数据与NCC和东部中南部造山带（ECAOB）的出版数据相结合，用于了解其培养和地壳生长和进化。在NCC的早期白垩纪火山岩显示出典型的大陆地壳的特点，阴性Nb和Ta异常，以及富集K和Pb。 NCC中的早期白垩纪火山岩的ε与分化指数相关（例如，MG＃），这意味着通过开放系统过程修改了地幔衍生的磁带。在NCC早期白垩纪火山岩中由高FO橄榄石托管的高Mg Closopogoxene和融化夹杂物具有更低的 207 </ sup> PB / 206 </ sup> PB和 208 </ sup> PB / 206 </ sup> PB比率比低橄榄石托管的低mg临床和熔体夹杂物，可以通过下地壳和玄武岩岩浆（岩浆混合或同化）之间的相互作用来解释。与NCC中的同疗法不同，ECAOB中的早期白垩纪火山岩具有高εnd值。除了ECAOB下方的少年下皮，还可以通过地壳同化和/或岩浆混合产生这些特征。早期白垩纪火山岩的“Adakitic”签名最有可能继承从较低的大陆地壳。较低地壳的大规模部分熔化可能已经与在延伸环境中连续的岩壁底层有关。这项工作表明，尽管具有“类似地壳”痕量的元素和同位素特征，所以中东亚洲的早期白垩纪火山岩代表了对地壳增长的不可止的贡献。 </ 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9期</span><b style="margin: 0 2px;">|</b><span>共15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=Qian Sheng‐Ping&option=202" target="_blank" rel="nofollow">Qian Sheng‐Ping;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Ren Zhong‐Yuan&option=202" target="_blank" rel="nofollow">Ren Zhong‐Yuan;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Le&option=202" target="_blank" rel="nofollow">Zhang Le;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Zhang Lei&option=202" target="_blank" rel="nofollow">Zhang Lei;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Wu Ya‐Dong&option=202" target="_blank" rel="nofollow">Wu Ya‐Dong;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Mei Sheng‐Wang&option=202" target="_blank" rel="nofollow">Mei Sheng‐Wang;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Xu Xiao‐Bo&option=202" target="_blank" rel="nofollow">Xu Xiao‐Bo;</a> <a href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Luo Qing‐Chen&option=202" target="_blank" rel="nofollow">Luo Qing‐Chen;</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>State Key Laboratory of Marine GeologyTongji UniversityShanghai China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry Guangzhou Institute of GeochemistryChinese Academy of SciencesGuangzhou China;</p> <p>State Key Laboratory of Isotope Geochemistry 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=Early Cretaceous volcanic rocks&option=203" rel="nofollow">Early Cretaceous volcanic rocks;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=Central‐East Asia&option=203" rel="nofollow">Central‐East Asia;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=crustal growth and evolution&option=203" rel="nofollow">crustal growth and evolution;</a> <a style="color: #3E7FEB;" href="/search.html?doctypes=4_5_6_1-0_4-0_1_2_3_7_9&sertext=assimilation and fractional crystallization (AFC) and magma mixing&option=203" rel="nofollow">assimilation and fractional crystallization (AFC) and magma mixing;</a> </p> <div class="translation"> 机译：早期白垩纪火山岩;中东亚洲;地壳增长和进化;同化和分数结晶（AFC）和岩浆混合; </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 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