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    Volume 48 Issue 10
    Oct.  2023
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    Article Navigation >  Earth Science  > 2023  >  48(10): 3631-3648
    Wang Zhenliang, Yang Jianzhou, Zhao Keqiang, Fu Yan'gang, Duan Zhuang, Lin Lujun, Xi Mingjie, Deng Youmao, Lu Guifu, 2023. Zircon U-Pb Age, Geochemical Characteristics and Geological Significance of Granite of Jiazishan Mo (Ag) Deposit, Inner Mongolia. Earth Science, 48(10): 3631-3648. doi: 10.3799/dqkx.2021.183
    Citation: Wang Zhenliang, Yang Jianzhou, Zhao Keqiang, Fu Yan'gang, Duan Zhuang, Lin Lujun, Xi Mingjie, Deng Youmao, Lu Guifu, 2023. Zircon U-Pb Age, Geochemical Characteristics and Geological Significance of Granite of Jiazishan Mo (Ag) Deposit, Inner Mongolia. Earth Science, 48(10): 3631-3648. doi: 10.3799/dqkx.2021.183
    shu

    Zircon U-Pb Age, Geochemical Characteristics and Geological Significance of Granite of Jiazishan Mo (Ag) Deposit, Inner Mongolia

    doi: 10.3799/dqkx.2021.183
    • 1.

      National Center for Geological Exploration Technology, Langfang 065000, China

    • 2.

      Institute of Geophysical and Geochemical Exploration, Chinese Academy of Geological Sciences, Langfang 065000, China

    • Received Date: 2021-08-10
      Available Online: 2023-10-31
    • Publish Date: 2023-10-25
      Abstract
    • The zircon LA-ICP-MS U-Pb age of the granite from the Jiazishan Mo (Ag) deposit in Inner Mongolia is 149.19±0.47 Ma, which is the product of Late Jurassic magmatism. The granite is characterized by high silicon (78.59%-80.58%), rich alkali (5.82%-6.34%), low P2O5 (0.002%-0.018%) and high Aluminium saturation index A/CNK (1.33-1.60), belongs to the high-K calc-alkaline series. The granite is enriched in trace elements Rb, K, La, Th, U, Hf, Pb, and depleted in trace elements Ba, Sr, Nb, Ta, Ti, P. The REE pattern shows a right-leaning enrichment type of LREE, with obvious negative Eu anomaly(0.25-0.49). The high differentiation index (DI) (91.87-94.30) and low solidification index (SI) (1.20-2.02) indicate that the rock has undergone the evolution of high differentiation and is a type of high differentiation I granite. The 176Hf/177Hf value is 0.282 96-0.282 96, the εHf(t) value is 7.82-9.86, and the two stage mode age (TDM2) is 744-929 Ma, suggesting that the granitic magma was formed by re-melting after the Neoproterozoic lower crust, which was formed by partial melting of depleted mantle material. The granite magma of Jiazishan and the Late Jurassic granite magma in the Da Hinggan Mountains were basically contemporaneous emplacement. The granite of Jiazishan may be related to the transformation of the tectonic environment from compression to post-collision extension after the closure of the Mongolia-Okhotsk Ocean, and superimposed influence by the subduction of the paleo-Pacific plate, which caused tectonic back-arc extension.

       

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