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    Volume 44 Issue 1
    Jan.  2019
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    Article Navigation >  Earth Science  > 2019  >  44(1): 234-247
    Li Zhidan, Li Xiaoguang, Cui Yurong, Li Guozhan, Zhang Jia, Guo Hu, Liu Wengang, Zhang Chao, Yu Reng'an, Xie Yu, Wang Jiaying, 2019. Yanshanian Mineralization of Zhaojinggou Nb-Ta Deposit, Inner Mongolia: Evidences from the Monazite and Zircon LA-MC-ICP-MS U-Pb and Biotite 40Ar-39Ar Geochronology. Earth Science, 44(1): 234-247. doi: 10.3799/dqkx.2018.100
    Citation: Li Zhidan, Li Xiaoguang, Cui Yurong, Li Guozhan, Zhang Jia, Guo Hu, Liu Wengang, Zhang Chao, Yu Reng'an, Xie Yu, Wang Jiaying, 2019. Yanshanian Mineralization of Zhaojinggou Nb-Ta Deposit, Inner Mongolia: Evidences from the Monazite and Zircon LA-MC-ICP-MS U-Pb and Biotite 40Ar-39Ar Geochronology. Earth Science, 44(1): 234-247. doi: 10.3799/dqkx.2018.100
    shu

    Yanshanian Mineralization of Zhaojinggou Nb-Ta Deposit, Inner Mongolia: Evidences from the Monazite and Zircon LA-MC-ICP-MS U-Pb and Biotite 40Ar-39Ar Geochronology

    doi: 10.3799/dqkx.2018.100
    • 1.

      Laboratory of Non-Fossil Energy Minerals, Tianjin Center of China Geological Survey, Tianjin 300170, China

    • 2.

      Beijing Research Institute of Uranium Geology, CNNC, Beijing 100029, China

    • Received Date: 2018-04-21
    • Publish Date: 2019-01-15
      Abstract
    • The Zhaojinggou Nb-Ta deposit is a newly explored large-scale deposit in Wuchuan County, Inner Mongolia. The Nb-Ta orebody is mainly hosted in the amazonite-bearing albite granite, and partly hosted in the granite aplite, greisen and amazonite granite pegmatite. In this paper, we use monazite and zircon LA-MC-ICP-MS U-Pb and biotite 40Ar-39Ar dating methods to constrain the mineralization age. Monazite LA-MC-ICP-MS U-Pb geochronological dating of four samples from granites yields ages of 124±2 Ma (MSWD=2.9, n=27), 124±3 Ma (MSWD=2.0, n=46), 121±1 Ma (MSWD=3.3, n=43) and 124±2 Ma (MSWD=3.2, n=12). One zircon sample from albite granite yields age of 125±1 Ma (MSWD=1.6, n=18). Meanwhile, biotite 40Ar-39Ar dating obtains the plateau age of 133.84±0.79 Ma (MSWD=3.31), isochron age of 134.55±0.79 Ma (MSWD=1.93) and reverse isochron age of 134.58±0.80 Ma (MSWD=1.99). Therefore, all these ages constrain that the ore-forming period of Zhaojinggou Nb-Ta deposit is Early Cretaceous. In conclusion, the Zhaojinggou deposit resulted from the tectonic-magmatic activities of extensional setting, and the Yanshanian Period is the main Nb-Ta metallogenic age in Inner Mongolia.

       

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