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安徽月山铜、金矿田成矿流体从深部向浅部沿断裂、裂隙以及多孔介质(含微裂隙)运移,运动速率分别为1.4m/s、9.8×10~(-1)～9.8×10~(-7)m/s、3.6×10~(-7)～4.6×10~(-7)m/s,流体运移通道介质性质的变化引起流体运移速率的变化是导致成矿物质在介质接触界面中沉淀的主要原因之一。成矿流体在高温时主要迁移方向向上,流体通量为n×10~4～n×10~5mol/cm~2,中低温时运移方向多样,大气降水介入岩浆热液体系导致流体通量增大,流体通量为n×10~5～n×10~6mol/cm~2;成矿流体中所携带的成矿物质具备形成大型铜矿床的潜力。
The ore-forming fluids migrate from deep to shallow along the faults and fissures and porous media (including microfractures) in the copper and gold fields of the Yueshan, Anhui Province at velocities of 1.4 m / s and 9.8 × 10 -1 to 9.8 × 10-7 m / s, and 3.6 × 10 -7 -6.6 × 10 -7 m / s. The change of the fluid properties of the fluid migration channel leads to the change of the fluid migration rate One of the main reasons for the precipitation of minerals in the media contact interface. The main migration direction of ore-forming fluid is upward at high temperature, the flux of fluid is n × 10 ~ 4 ~ n × 10 ~ 5mol / cm ~ 2, and the migration direction is diversified in low and medium temperature. The fluid flux is n × 10 ~ 5 ~ n × 10 ~ 6mol / cm ~ 2. The ore-forming materials carried in the ore-forming fluid have the potential of forming large copper deposits.