首页> 外文期刊>Precambrian Research >Middle Neoproterozoic (similar to 845 Ma) continental arc magmatism along the northwest side of the Jiangshan-Shaoxing suture, South China: Geochronology, geochemistry, petrogenesis and tectonic implications
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Middle Neoproterozoic (similar to 845 Ma) continental arc magmatism along the northwest side of the Jiangshan-Shaoxing suture, South China: Geochronology, geochemistry, petrogenesis and tectonic implications

机译:中国南方江山—绍兴缝合线西北侧的中新元古代(类似于845 Ma)大陆弧岩浆作用:年代学,地球化学,成岩作用和构造意义

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This paper presents the first detailed zircon U-Pb chronology, major and trace element, and Nd-Hf isotope geochemistry of two Neoproterozoic plutons (Shanhou and Jiangshan) along the northwest side of the Jiangshan-Shaoxing suture, Zhejiang province, South China. The Shanhou pluton consists of gabbros, dioritic rocks and monzogranites. SHRIMP and LA-ICP-MS zircon U-Pb dating indicates that the gabbros (similar to 846 Ma), dioritic rocks (similar to 845 Ma) and monzogranites (similar to 847 Ma) were emplaced simultaneously. The Jiangshan pluton consists mainly of dioritic rocks that were also emplaced in the middle Neoproterozoic with a SHRIMP zircon U-Pb age of ca. 842 Ma. The Shanhou gabbros are mainly high-K calc-alkaline, and are enriched in LREE and LILE and depleted in HFSE with marked negative Ta-Nb anomalies. They have positive epsilon(Nd) (T) (2.0-3.5) and epsilon(Hf) (T) (in-situ zircon) (3.3). The Shanhou and Jiangshan dioritic rocks as well as the Shanhou granites are also high-K calc-alkaline, enriched in LREE and LILE and depleted in HFSE with marked negative Ta-Nb anomalies. They also show positive epsilon(Nd) (T) (0.1-4.7) and epsilon(Hf) (T) (in-situ zircon) (0.8-5.0). Detailed elemental and isotopic data suggest that both plutons were formed in a continental arc setting with gabbros derived from partial melting of subduction-modified mantle wedge. Such gabbroic magmas underwent fractionation crystallization of clinopyroxene + amphibole, forming the less felsic dioritic rocks. Progressive fractionation crystallization of amphibole + plagioclase from the evolved melts with a little crustal assimilation produced the more felsic dioritic rocks and granites. Our new data suggest that final amalgamation between the Yangtze and Cathaysia blocks postdated 842 Ma. (C) 2015 Elsevier B.V. All rights reserved.
机译:本文介绍了中国浙江省江山—绍兴缝合线西北侧两个新元古代岩体(山后和江山)的第一个详细的锆石U-Pb年代,主要和微量元素以及Nd-Hf同位素地球化学。山后岩体由辉长岩,闪长岩和辉长岩组成。 SHRIMP和LA-ICP-MS锆石U-Pb测年表明,辉长岩(约846 Ma),闪长岩(约845 Ma)和辉长岩(约847 Ma)同时存在。江山岩体主要由闪长岩组成,这些闪长岩也被置于新元古代中期,SHRIMP锆石的U-Pb年龄约为。 842马汕侯长尾小猴主要是高钾钙碱性物质,富含LREE和LILE,贫乏HFSE,Ta-Nb异常明显。他们的正epsilon(Nd)(T)(2.0-3.5)和epsilon(Hf)(T)(原位锆石)(3.3)为正。山厚和江山闪长岩以及山厚花岗岩也是高K钙碱性矿床,富含LREE和LILE,而HFSE贫化,Ta-Nb异常明显。他们还显示出正ε(Nd)(T)(0.1-4.7)和ε(Hf)(T)(原位锆石)(0.8-5.0)。详细的元素和同位素数据表明,两种俯冲体都是在大陆弧环境中形成的,辉长岩来自俯冲修饰的地幔楔的部分熔融。此类辉长岩岩浆经历了次氯环己烯+闪石的分馏结晶,形成了较稀疏的闪长岩。闪石和斜长石的逐步分馏结晶从逐渐融化的熔体中经过少量的地壳同化,产生了更多的长英质闪长岩和花岗岩。我们的新数据表明,长江和华夏地块之间的最终合并发生在842 Ma之后。 (C)2015 Elsevier B.V.保留所有权利。

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