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Zircon U-Pb ages of the two-periods magmatism from the Xiuwacu Mo-W-Cu deposit, northwest Yunnan, China

         

摘要

The Xiuwacu deposit is a large magmatic hydrothermal Mo-W-Cu deposit, and also a typical representative of the late Triassic mineralization in Geza Arc (Lai AQ et al., 2016;Liu XL et al., 2017). The Xiuwacu pluton intruded into the Lamaya Formation, and contains two periods of rocks bounded by intrusive contact. Nonetheless, most of the intrusive boundaries were superposed by later fault structures.

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  • 来源
    《中国地质(英文)》 |2019年第003期|391-392|共2页
  • 作者单位

    Guilin University of Technology Guilin 541004 China;

    Sichuan Geological Survey Chengdu 610081 China;

    Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province Chengdu 610081 China;

    Sichuan Geological Survey Chengdu 610081 China;

    Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province Chengdu 610081 China;

    Sichuan Geological Survey Chengdu 610081 China;

    Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province Chengdu 610081 China;

    Sichuan Geological Survey Chengdu 610081 China;

    Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province Chengdu 610081 China;

    Sichuan Geological Survey Chengdu 610081 China;

    Evaluation and Utilization of Strategic Rare Metals and Rare Earth Resource Key Laboratory of Sichuan Province Chengdu 610081 China;

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