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    Volume 47 Issue 9
    Sep.  2022
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    Article Navigation >  Earth Science  > 2022  >  47(9): 3127-3146
    Zhang Lianchang, Feng Jing, Li Ping, Zhu Mingtian, Dong Zhiguo, Gao Bingyu, Zhang Xin, Wang Changle, Chen Bo, Ji Wenhua, 2022. Tectonic Evolution and Metallogenic Regularity of Dominant Deposits in the Western Tianshan. Earth Science, 47(9): 3127-3146. doi: 10.3799/dqkx.2021.222
    Citation: Zhang Lianchang, Feng Jing, Li Ping, Zhu Mingtian, Dong Zhiguo, Gao Bingyu, Zhang Xin, Wang Changle, Chen Bo, Ji Wenhua, 2022. Tectonic Evolution and Metallogenic Regularity of Dominant Deposits in the Western Tianshan. Earth Science, 47(9): 3127-3146. doi: 10.3799/dqkx.2021.222
    shu

    Tectonic Evolution and Metallogenic Regularity of Dominant Deposits in the Western Tianshan

    doi: 10.3799/dqkx.2021.222
    • 1.

      Key Laboratory of Mineral Resources, Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China

    • 2.

      University of Chinese Academy of Sciences, Beijing 100049, China

    • 3.

      Xinjiang Bureau of Geology and Mineral Resources and Development, Urumqi 830000, China

    • 4.

      Xi'an Center of Geological Survey, China Geological Survey, Xi'an 710054, China

    • Received Date: 2021-11-24
    • Publish Date: 2022-09-25
      Abstract
    • The West Tianshan is located in the southwest margin of the Central Asian accretionary orogenic belt. It is sandwiched between Junggar Block and Tarim Craton. Its tectonic evolution is closely related to subduction-closed processes of Tianshan ocean. The geological structure of the West Tianshan is complex and its mineralization is unique. Some ore concentration areas were developed in West Tianshan orogen, such as porphyry gold-copper deposit and volcanic-sedimentary type ferromanganese deposit related to active continental margin, and submarine hydrothermal sedimentary lead-zinc deposit and epithermal hydrothermal gold deposit related to extensional tectonics setting. The tectonic evolution and mineralization of the West Tianshan have always been the focus of geological research. In recent years, significant progress has been made in geological prospecting and basic research. However, there are still some major geological and ore-forming problems to be solved urgently. Based on comprehensive study of the regional geological background, sedimentary formation, magmatic evolution, metallogenic geological characteristics, ore-forming material sources and ore-controlling factors, it is shown that West Tianshan orogen has experienced some geodynamic processes, namely the formation of Precambrian continent, ocean-continent subduction accretion, continent-continent collision orogen. Some main metallogenic belts were formed in the West Tianshan from Precambrian to Late Paleozoic, such as (1) Haldaban Precambrian Pb-Zn metallogenic belt, (2) Borokonu Paleozoic gold⁃copper⁃lead-zinc polymetallic metallogenic belt, (3) Awulale Late Paleozoic iron manganese polymetallic metallogenic belt, (4) Nalati Paleozoic gold-copper polymetallic metallogenic belt. And on that basis, some the ore-forming models of the main metallogenic belts were established, the metallogenic sequences related to sedimentary formation-tectonic-magmatic activity were determined, the spatiotemporal structural models of the regional dominant resources such as iron, copper, lead, zinc and gold were summarized.

       

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