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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): 1454-1471
    Lin Bin, Wang Liqiang, Tang Juxing, Song Yang, Zhou Xin, Liu Zhibo, Gao Yiming, Tang Xiaoqian, Xu Ruige, Chen Zaojun, 2017. Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet. Earth Science, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517
    Citation: Lin Bin, Wang Liqiang, Tang Juxing, Song Yang, Zhou Xin, Liu Zhibo, Gao Yiming, Tang Xiaoqian, Xu Ruige, Chen Zaojun, 2017. Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet. Earth Science, 42(9): 1454-1471. doi: 10.3799/dqkx.2017.517
    shu

    Zircon U-Pb Geochronology of Ore-Bearing Porphyries in Baomai Deposit, Yulong Copper Belt, Tibet

    doi: 10.3799/dqkx.2017.517
    • 1.

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

    • 2.

      Centre of Excellence in Ore Deposit, University of Tasmania, Hobart 7001, Australia

    • 3.

      Geothermal Geological Survey Party, Tibet Bureau of Geology and Mineral Exploration and Development, Lhasa 850000, China

    • 4.

      China Mining Federation of Beijing Consulting Center, Bejing 100044, China

    • 5.

      Tibet Dachuan Mining Limited Company, Lhasa 850000, China

    • 6.

      Tibet Yilong Mining Limited Company, Lhasa 850000, China

    • Received Date: 2016-11-22
    • Publish Date: 2017-09-15
      Abstract
    • Baomai porphyry copper-molybdenite deposit is an important part of the northern Yulong copper belt, Tibet, with typical porphyry-type mineralization and alteration. The latest exploration shows that both Cu and Mo resources have reached the medium-sized deposit, but the research work is still very poor. Based on the basic geological characteristics, intrusion ages of biotite granite porphyry and biotit-monzogranite are 41.3±0.2 Ma and 40.8±0.2 Ma, respectively, according to the LA-ICP-MS zircon U-Pb geochronology method. These results are consistent with those of Yulong and Zhanaga deposits. All of them are the products of continent collision orogeny of India with Eurasia in Eocene. Geochronology evidences show that porphyries related to mineralization in the Yulong copper belt are mainly intruded at 37-42 Ma, and no obviously early (51 Ma), medium (41 Ma) and late (33 Ma) stages magmatic activities. From northwest to southeast, the ages of diagenesis and mineralization in Yulong copper belt do not change to be younger significantly.

       

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