Geochronology and geochemistry of late Jurassic adakitic intrusions and associated porphyry Mo–Cu deposit in the Tongcun area, east China: Implications for metallogenesis and tectonic setting | |
Yanwen Tang; Xiaofeng Li; Yuling Xie; Liang Liu; Tingguang Lan; Sebastien Meffre; Cheng Huang | |
刊名 | Ore Geology Reviews |
2017 | |
卷号 | 80页码:289-308 |
关键词 | Qinzhou–hangzhou Metallogenic Belt High–k Calc–alkaline I–type Granite Zircon U–pb Dating Sericite Ar–ar Dating Tongcun Adakitic Intrusions |
英文摘要 | The genesis of adakites and associated Mo–Cu mineralization in non–arc settings in China is poorly constrained. Here, we present geochronology, geochemistry and Sr–Nd–Pb isotopes for the Tongcun intrusive complex, and report Pb isotopes and 40Ar–39Ar age for the Tongcun Mo–Cu deposit. The Tongcun intrusive complex is composed mainly by granodiorite and monzogranite (phase 1 and phase 2), with emplacement age of 160 Ma to 148 Ma. The Tongcun complex can be classified as typical high–K calc–alkaline I–type granitoid and also shows adakitic geochemical features. Moreover, the negative Nb, Ta, Ti, and P anomalies and enriched initial 87Sr/86Sr ratios of 0.7083–0.7092 of the Tongcun intrusive complex are consistent with those of the subduction–related magmatism. The 40Ar–39Ar dating of sericite, which is intergrown with chalcopyrite, indicates that the late Cu mineralization event occurred at ~ 155.5 Ma. The early Mo (Cu) and the late Cu mineralization events in this deposit were temporally, spatially and genetically associated with the emplacement of monzogranite (phase 1). There are no obvious linear correlation between SiO2 and most of the major and trace elements, and all rock samples fall within the fields of unfractional crystallization felsic granites in Zr + Nb + Ce + Y versus FeOT/MgO and (K2O + Na2O)/CaO diagrams, indicating that partial melting rather than fractional crystallization has played an important role for the formation of the Tongcun intrusive complex. Magmatic inherited zircons from the Tongcun granitoids with the age peaked at 780–812 Ma, imply that the Neoproterozoic igneous rocks in the lower crust have been incorporated into the magma source. The uniform εNd(t) (− 6.3 to − 7.3), initial 87Sr/86Sr, 207Pb/204Pb (15.596–15.621), and 208Pb/204Pb (38.374–38.650), as well as high K2O contents (3.36–4.10 wt.%) and relatively high Mg# values (35.40 to 40.30) suggest the Tongcun intrusive complex was derived from partial melting of the thickened lower continental crust triggered by basaltic magma underplating plus additional input from the EM II mantle-derived basaltic melts. The Tongcun area was controlled by a compression setting related to the subduction of the Paleo–Pacific Plate in Mesozoic period. |
语种 | 英语 |
内容类型 | 期刊论文 |
源URL | [http://ir.gyig.ac.cn/handle/42920512-1/8394] |
专题 | 地球化学研究所_矿床地球化学国家重点实验室 |
作者单位 | 1.School of Civil and Environmental Engineering, University of Science and Technology Beijing, Beijing 100083, China 2.CODES ARC Centre of Excellence in Ore Deposits, University of Tasmania, Hobart, TAS 7001, Australia 3.State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China 4.Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China |
推荐引用方式 GB/T 7714 | Yanwen Tang;Xiaofeng Li;Yuling Xie;Liang Liu;Tingguang Lan;Sebastien Meffre;Cheng Huang. Geochronology and geochemistry of late Jurassic adakitic intrusions and associated porphyry Mo–Cu deposit in the Tongcun area, east China: Implications for metallogenesis and tectonic setting[J]. Ore Geology Reviews,2017,80:289-308. |
APA | Yanwen Tang;Xiaofeng Li;Yuling Xie;Liang Liu;Tingguang Lan;Sebastien Meffre;Cheng Huang.(2017).Geochronology and geochemistry of late Jurassic adakitic intrusions and associated porphyry Mo–Cu deposit in the Tongcun area, east China: Implications for metallogenesis and tectonic setting.Ore Geology Reviews,80,289-308. |
MLA | Yanwen Tang;Xiaofeng Li;Yuling Xie;Liang Liu;Tingguang Lan;Sebastien Meffre;Cheng Huang."Geochronology and geochemistry of late Jurassic adakitic intrusions and associated porphyry Mo–Cu deposit in the Tongcun area, east China: Implications for metallogenesis and tectonic setting".Ore Geology Reviews 80(2017):289-308. |
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