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    Volume 43 Issue 12
    Dec.  2018
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    Article Navigation >  Earth Science  > 2018  >  43(12): 4638-4650
    Chen Wei, Mao Jingwen, Xu Zhaowen, Qu Xiaoming, Yu Yang, 2018. Two Stages of Cretaceous Granitic Magmatisms and Mo Mineralizations in West Dabie Orogenic Belt. Earth Science, 43(12): 4638-4650. doi: 10.3799/dqkx.2018.522
    Citation: Chen Wei, Mao Jingwen, Xu Zhaowen, Qu Xiaoming, Yu Yang, 2018. Two Stages of Cretaceous Granitic Magmatisms and Mo Mineralizations in West Dabie Orogenic Belt. Earth Science, 43(12): 4638-4650. doi: 10.3799/dqkx.2018.522
    shu

    Two Stages of Cretaceous Granitic Magmatisms and Mo Mineralizations in West Dabie Orogenic Belt

    doi: 10.3799/dqkx.2018.522
    • 1.

      Key Laboratory of Metallogeny and Mineral Assessment, Ministry of Natural Resources, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China

    • 2.

      School of Earth Science and Engineering, Nanjing University, Nanjing 210093, China

    • 3.

      Economic Research Institute, Ministry of Natural Resources, Langfang 065200, China

    • Received Date: 2018-04-24
    • Publish Date: 2018-12-15
      Abstract
    • This paper investigates the petrogenesis of the Cretaceous Mo-bearing granites in West Dabie orogenic belt. Utilizing the rock geological chemistry of these granites, the formation condition of the Mo deposits in West Dabie orogen is discussed, which is significant to recognize the geochemical dynamics background of West Dabie Mo metallogenic belt. Similar to the Cretaceous granites in East Dabie orogen, the magmatisms of Mo-bearing granites in West Dabie orogen could be divided into two stages. The early stage was formed under thickened crustal environment, and the late stage was formed under non-thickened crustal environment. This is fundamental reason to decide the differences of the Mo metallization in West Dabie orogen. Combining with the geochemical characteristics of the Mo and the evolutionary process of central orogenic belt, the Qinling paleo-oceanic basin probably offered a favorable environment for the supergene weathering crustal Mo element, and then the Mo enriched sediment was carried by the Yangtze block and subducted underneath the North China block. Together with the Yangtze block, the Mo enriched sediment was partial melted, forming the large-scale Mo-bearing magmatism in West Dabie orogen.

       

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