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    Volume 45 Issue 3
    Mar.  2020
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    Article Navigation >  Earth Science  > 2020  >  45(3): 910-929
    Wu Haoran, Xie Yuling, Zhong Richen, Wang Ying, 2020. Geochronology, Geochemistry and Geological Significance of the Syeno-Granite Porphyry from Yinshuisi Pb-Zn Deposit, Dabie Orogenic Belt. Earth Science, 45(3): 910-929. doi: 10.3799/dqkx.2019.070
    Citation: Wu Haoran, Xie Yuling, Zhong Richen, Wang Ying, 2020. Geochronology, Geochemistry and Geological Significance of the Syeno-Granite Porphyry from Yinshuisi Pb-Zn Deposit, Dabie Orogenic Belt. Earth Science, 45(3): 910-929. doi: 10.3799/dqkx.2019.070
    shu

    Geochronology, Geochemistry and Geological Significance of the Syeno-Granite Porphyry from Yinshuisi Pb-Zn Deposit, Dabie Orogenic Belt

    doi: 10.3799/dqkx.2019.070

    • School of Civil and Resources Engineering, University of Science and Technology Beijing, Beijing 100083, China

    • Received Date: 2019-01-29
    • Publish Date: 2020-03-15
      Abstract
    • The Yinshuisi Zn-Pb deposit,located in the north border of Dabie Orogen Belt,Jinzhai County,Anhui Province,is the largest skarn deposit in the Dabieshan region. Previous studies on chronology,geochemistry and petrogenesis of intrusions are few,which has restricted the understanding of lead-zinc metallogenic regularity. Detailed geochronology,geochemistry,and isotopic data for ore-related syeno-granite were analyzed in this study.LA-ICP-MS U-Pb dating of zircon from Yinshuisi syeno-granite porphyry yields age of 125.4±0.4 Ma,suggesting that it resulted from Early Cretaceous magmatism.According to the geochemical analysis,Yinshuisi syeno-granite porphyry has high SiO2 (71.43%-72.71%),K2O (4.62%-4.88%) and ALK (K2O+Na2O=7.47%-7.81%),but weakly peraluminous (A/CNK=1.03-1.06). The rock is enriched in Fe,Rb,Th,U and LREE,depleted in Ca,Sr,Ba,Ti,P and HREE with negative Eu anomalies,which indicates that Yinshuisi syeno-granite porphyry belongs to aluminous A-type granite.The Yinshuisi syeno-granite porphyry has highly enriched Sr-Nd-Hf isotopic compositions: (87Sr/86Sr)i=0.710 21-0.710 53,εNd(t)=-20.0—-19.2. The εHf(t) value ranges from -26.7 to -23.8,lying below the depleted mantle line.The TDM2 value ranges from 2 663 Ma to 2 845 Ma,which indicates that the syeno-granite porphyry derived from dominantly the mixing of Yangtze's lower crust with the Dabie Complex. Yinshuisi syeno-granite porphyry was emplaced after the major collisional period of the North China Block and Yangtze Block,in a post-collisional or intracontinental extensional setting under the regional extension mechanism,which has the capacity to cause the regional upwelling of the asthenospheric mantle. The thinned lithospheric mantle was exposed to the upwelling asthenopsheric mantle,leading to intensive magmatism,which was related to the rollback of westward subducting Paleo-Pacific Plate beneath the Asian continent.

       

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