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 int...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.展开更多
文摘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.
