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通过金管冲铀矿床成矿构造背景和矿田构造的多尺度解析,系统论述了不同尺度的构造对成矿的控制作用.结合成矿流体的物理化学性质,探讨了矿床的形成机制.以上研究反映了“构造场地准备→富铀岩体形成→成矿流体演化→成矿元素沉淀”这一动态过程.
Based on the multi-scale analysis of metallogenic tectonic setting and ore-field structure of the Jin-Guanchong uranium deposit, systematically discusses the control effect of different scale structures on mineralization, and discusses the formation mechanism of the ore deposit in combination with the physico-chemical properties of ore- It reflects the dynamic process of “preparation for formation site → formation of uranium-rich rock mass → evolution of ore-forming fluid → precipitation of ore-forming elements”.