The faults controlled the mineralization mainly and connected the deep with the surface by the upward migration of the deep-derived auriferous metallogenetic fluids via the fractured zones and by their later precipitation.
英
美
释义
提出了断裂构造对成矿的主要控制作用,它起着沟通深部与浅部的作用,并使深部的含金流体沿断裂破碎带上升、沉淀而成矿。
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