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.

• 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。