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    中国百强科技报刊

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    Volume 42 Issue 9
    Sep.  2017
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    Article Navigation >  Earth Science  > 2017  >  42(9): 1441-1453
    Zheng Youye, Ci Qiong, Wu Song, Jin Liangxu, Guo Jianci, Ci Renji, Gong Fuzhi, Tan Meng, Zhang Hongqiang, 2017. The Discovery and Significance of Rongga Porphyry Mo Deposit in the Bangong-Nujiang Metallogenic Belt, Tibet. Earth Science, 42(9): 1441-1453. doi: 10.3799/dqkx.2017.109
    Citation: Zheng Youye, Ci Qiong, Wu Song, Jin Liangxu, Guo Jianci, Ci Renji, Gong Fuzhi, Tan Meng, Zhang Hongqiang, 2017. The Discovery and Significance of Rongga Porphyry Mo Deposit in the Bangong-Nujiang Metallogenic Belt, Tibet. Earth Science, 42(9): 1441-1453. doi: 10.3799/dqkx.2017.109
    shu

    The Discovery and Significance of Rongga Porphyry Mo Deposit in the Bangong-Nujiang Metallogenic Belt, Tibet

    doi: 10.3799/dqkx.2017.109
    • 1.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083, China

    • 2.

      School of Earth Science and Resources, China University of Geosciences, Beijing 100083, China

    • 3.

      State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Wuhan 430074, China

    • 4.

      No.2 Geological Party, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Lhasa 850000, China

    • 5.

      Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Lhasa 850000, China

    • 6.

      No.6 Geological Party, Tibet Autonomous Region Geological and Mineral Exploration and Development Bureau, Deqing, Lhasa 851400, China

    • Received Date: 2016-12-05
    • Publish Date: 2017-09-15
      Abstract
    • The Bangong-Nujiang metallogenic belt is a new discovery with obvious prospecting breakthrough in the last ten years, mainly including porphyry-skarn and porphyry-hypothermal types Cu-Au deposits, which are poorly studied. The Rongga deposit located at the western segment of south Bangong-Nujiang suture zone, is the first porphyry Mo deposit discovered in 2016 that has a perspective large scale in the Bangong-Nujiang metallogenic belt. The Rongga deposit yielded a molybdenite Re-Os weighted mean age of 99.3±0.1 Ma (MSWD=0.2, n=8), consistent with the isochron age of 99.2±0.4 Ma (MSWD=0.2, n=8), which indicated the mineralization occurred at early stage of Late Cretaceous during the collision between Lhasa and Qiangtang terranes when the subducted Bangong-Nujiang oceanic crust has closed. This discovery of Rongga deposit has enriched the knowledge of metallogenic theory, filled the gap of Mo resources in this region, and the existed models are challenged in the Bangong-Nujiang belt. This discovery of Rongga deposit show the potential for porphyry Mo mineralization along the Bangong-Nujiang suture zone, and provide an example illustration and theoretical support for further exploration of porphyry Mo deposit in this belt.

       

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