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    Volume 45 Issue 1
    Jan.  2020
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    Xie Yuanhui, Li Xiaowei, Zhu Xinyou, Huang Xingkai, Liu Teng, Xu Qiao, Liu Zi, 2020. Petrogenesis and Mineralization Chronology Study on the Mo Deposit of the Haisugou Intrusive Mass, Inner Mongolia, and Its Geological Implications. Earth Science, 45(1): 43-60. doi: 10.3799/dqkx.2018.341
    Citation: Xie Yuanhui, Li Xiaowei, Zhu Xinyou, Huang Xingkai, Liu Teng, Xu Qiao, Liu Zi, 2020. Petrogenesis and Mineralization Chronology Study on the Mo Deposit of the Haisugou Intrusive Mass, Inner Mongolia, and Its Geological Implications. Earth Science, 45(1): 43-60. doi: 10.3799/dqkx.2018.341

    Petrogenesis and Mineralization Chronology Study on the Mo Deposit of the Haisugou Intrusive Mass, Inner Mongolia, and Its Geological Implications

    doi: 10.3799/dqkx.2018.341
    • Received Date: 2018-09-26
    • Publish Date: 2020-01-15
    • The Haisugou rock mass is located in the southern part of the Daxing'anling orogenic belt. The Haisugou Mo deposit and the Xiaojingzibei Cu and Mo deposit are found in the intrusive mass. At present,the understanding of the rock mass is insufficient,the genetic type is controversial and the difference between the two molybdenum deposits has not been discussed. In this study,zircon U-Pb geochronology and petro-geochemistry analyses were carried out on different rocky granites in Haisugou rock mass,and Re-Os isotope analyses on molybdenite in the mining area were conducted. The LA-ICP-MS zircon U-Pb dating results of the biotite granite in the Haisugou molybdenum mining area are 137.1±0.6 Ma and 143.6±0.8 Ma; the Re content of molybdenite in the Haisugou molybdenum deposit is 2.1×10-6,the molybdenite Re-Os model age is 143.9±2.9 Ma. The dating result of LA-ICP-MS zircon U-Pb of the monzonitic granite in the Xiaojingzibei copper-molybdenum deposit is 126.5±0.7 Ma.The granite in the Haishugou pluton belongs to high-K calc-alkaline series Ⅰ-type granite with metaluminous to weakly peraluminous characteristics. The main elements SiO2 content is 68.81%-77.18%,K2O+Na2O=6.80%-8.31%,CaO content ranges from 0.43% to 2.88%,MgO ranges from 0.15% to 1.32% and aluminum index (A/CNK) value ranges from 0.97 to 1.07. The rocks are relatively enriched in light rare-earth elements (La/Yb)N=6.19-10.74 and the rare earth distribution pattern is right-dipping with a moderate negative Eu anomalies with a δEu value from 0.37 to 0.81. By combining existing research results,It can be considered that the magma evolution experienced magma mixing and the fractional crystallization plays a dominant role. The time of diagenesis and molybdenum metallogenesis of the Haisugou intrusive mass coincides with the time of the third phase of the large-scale diagenesis and mineralization of the Silamulun metallogenic belt,indicating the corresponding tectonic background is the transition of the tectonic system (from the extrusion environment to the tensile environment) to the lithosphere thinning environment.

       

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