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    Volume 48 Issue 10
    Oct.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(10): 3725-3742
    Cui Kai, Xie Yuling, Qu Yunwei, Tang Yanwen, Li Lamei, Chen Qi, 2023. Geochemistry, Geochronology and Petrogenesis of Granite Porphyry in Langcun W-Mo Deposit, Zhejiang Province. Earth Science, 48(10): 3725-3742. doi: 10.3799/dqkx.2021.209
    Citation: Cui Kai, Xie Yuling, Qu Yunwei, Tang Yanwen, Li Lamei, Chen Qi, 2023. Geochemistry, Geochronology and Petrogenesis of Granite Porphyry in Langcun W-Mo Deposit, Zhejiang Province. Earth Science, 48(10): 3725-3742. doi: 10.3799/dqkx.2021.209
    shu

    Geochemistry, Geochronology and Petrogenesis of Granite Porphyry in Langcun W-Mo Deposit, Zhejiang Province

    doi: 10.3799/dqkx.2021.209
    • 1.

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

    • 2.

      State Key Laboratory of Ore Deposit Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550081, China

    • 3.

      Institute of Mineral Resources Research, China Metallurgical Geology Bureau, Beijing 101300, China

    • 4.

      No. 1 Geological Exploration Unit of Zhejiang Province, Hangzhou 310012, China

    • Received Date: 2021-09-03
      Available Online: 2023-10-31
    • Publish Date: 2023-10-25
      Abstract
    • The Langcun tungsten-molybdenum deposit is a medium porphyry-skarn type deposit in the Northwest Zhejiang Province, western Qinzhou-Hangzhou metallogenic belt (QHMB). In this paper, it analyzed the petrological, chronological and geochemical characteristics of the ore-forming related granite porphyry in this deposit to constrain its genesis and interpret its tectonic significance. Granite porphyry formed at 129.7±1.1 Ma (zircon U-Pb, LA-ICP-MS) and belongs to shoshonite series with high SiO2, alkali contents, and weakly peraluminous. The characteristics, i.e., right-dipping chondrite normalized REE pattern with negative Eu anomalies (δEu=0.36-0.40) and the 10 000 Ga/Al and Zr+Nb+Ce+Y values range from 2.57 to 2.90 and 379.5×10-6 to 462.0×10-6, respectively, suggest that the granite porphyry belongs to A-type granite. Whole rock Sr-Nd compositions are characterized by ISr and εNd(t) range from 0.707 17 to 0.709 08 and -6.1 to -4.0, respectively, with Nd model ages of 1.25 to 1.42 Ga. Meanwhile, zircon Hf compositions are characterized by εHf(t)=-5.94 to -0.87 with two stage model ages of 1.23 to 1.56 Ga. All these evidences suggest that granite porphyry is formed by an ancient continental crust mixed with mantle material source under the tectonic of lithosphere extension and thinning in South China.

       

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