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    Volume 45 Issue 4
    Apr.  2020
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    Yu Junzhen, Zheng Youye, Xu Rongke, Hou Weidong, Cai Pengjie, 2020. Zircon U-Pb Chronology, Geochemistry of Jiangjunmu Ore-Bearing Pluton, Eastern Part of East Kunlun and Their Geological Significance. Earth Science, 45(4): 1151-1167. doi: 10.3799/dqkx.2019.134
    Citation: Yu Junzhen, Zheng Youye, Xu Rongke, Hou Weidong, Cai Pengjie, 2020. Zircon U-Pb Chronology, Geochemistry of Jiangjunmu Ore-Bearing Pluton, Eastern Part of East Kunlun and Their Geological Significance. Earth Science, 45(4): 1151-1167. doi: 10.3799/dqkx.2019.134

    Zircon U-Pb Chronology, Geochemistry of Jiangjunmu Ore-Bearing Pluton, Eastern Part of East Kunlun and Their Geological Significance

    doi: 10.3799/dqkx.2019.134
    • Received Date: 2019-06-06
    • Publish Date: 2020-04-15
    • Jiangjunmu ore-bearing granodiorite porphyry is located in the eastern part of East Kunlun orogenic belt. In this paper,zircon U-Pb dating and Lu-Hf isotopes,whole-rock major and trace elements of ore-bearing granodiorite porphyry are presented to discuss their geochronology and genesis. The results show that the ore-bearing granodiorite porphyry was formed at the Late Triassic with the age of 218.8±1.3 Ma. It has contents of SiO2(65.23%-67.25%),MgO(1.50%-1.59%),Al2O3(15.30%-15.75%) with K2O/Na2O ratios ranging from 1.00 to 1.20 and Mg# values ranging from 43 to 44. The ore-bearing granodiorite porphyries are characterized by high silicon,aluminum and high-potassium,belonging to the high-potassium rock. Meanwhile,they are enriched in large ion lithophile elements (LILEs) such as Th,U,Rb and K,and depleted in high field strength elements (HFSE) such as Nb,P and Zr. Hf isotopic compositions of the ore-bearing granodiorite porphyry (εHf(t)=-1.7-+1.01,TDM2=1 064-1 214 Ma),indicating that their parental magmas were derived from the Middle Proterozoic lower crust. Coupled with the petrography of a small number of mafic microgranular enclaves,geochronology,petrology and geochemistry data indicate that ore-bearing granodiorite porphyry originated from the mixing of dominating re-melting of Middle Proterozoic lower crust and a small amount of mantle-derived materials. The ore-bearing granodiorite porphyry was formed in the post-collisional orogenic extensional setting,indicative of the crust-mantle diagenesis and mineralization at Late Triassic in the East Kunlun. It is not only the product of the Paleo-Tethys tectonic and magmatic event in the East Kunlun,but also has good metallogenic conditions,which provides important evidence for the study of the Late Triassic magmatism in the East Kunlun and search for porphyry or hydrothermal polymetallic deposits.

       

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