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    中国百强科技报刊

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    中国高校百佳科技期刊

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    Volume 45 Issue 8
    Aug.  2020
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    Article Contents
    Geng Quanru, Zhang Zhang, Peng Zhimin, Guan Junlei, Cong Feng, 2020. Petrogeochemistry and Metallogenesis Related to Xiongmei-Baingoin Granitic Zone in Central Tibet. Earth Science, 45(8): 2805-2825. doi: 10.3799/dqkx.2020.204
    Citation: Geng Quanru, Zhang Zhang, Peng Zhimin, Guan Junlei, Cong Feng, 2020. Petrogeochemistry and Metallogenesis Related to Xiongmei-Baingoin Granitic Zone in Central Tibet. Earth Science, 45(8): 2805-2825. doi: 10.3799/dqkx.2020.204

    Petrogeochemistry and Metallogenesis Related to Xiongmei-Baingoin Granitic Zone in Central Tibet

    doi: 10.3799/dqkx.2020.204
    • Received Date: 2020-06-17
    • Publish Date: 2020-08-15
    • The continuous Xiongmei-Baingoin-Qinglong-Sangxiong granite zone, located in central Tibet, belongs to the middle part of the Bangong-Nujiang metallogenic belt. Small- and medium-sized deposits were discovered in recent years, such as Xiongmei, Kuga, Ri'a copper deposits and Qinglong lead-zinc deposit, but no bigger deposits were found in this zone. Based on comprehensive data collection and field investigation, research on geochemical properties, magma sources and ore-forming factors of the granitic zone was carried out. The granitic intrusive stages can be identified at 140-125 Ma, 120-110 Ma, 94-72 Ma, and some Cenozoic intrusions, with a magmatic flare-up at 120-110 Ma. In western part of this area, the Early Cretaceous Shesuo, Xiongmei, Kuga granitic intrusives and the Late Cretaceous Xueru, and Sangxinri granitic intrusives are significant ore-forming granites with copper, gold and iron deposits. However, they are different from granitic intrusives forming super-large porphyry copper deposits regarding to their magma sources and surrounding rock. They have prospecting potential to form medium- or large-sized porphyry copper, gold deposits or skarn-type deposits similar to the Qingcaoshan copper deposit. The Early Cretaceous granites distributed continuously along Baingoin, Qinglong and Sangxiong are closely related to hydrothermal and skarn-type iron, lead and zinc polymetallic mineralization.

       

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