It is concluded that the fluid forming this type of copper-gold deposit is one high oxygen and sulphur fugacity and low-to-moderate temperature acid fluid.
认为形成这一类型矿床的流体是一种高氧逸度、高硫逸度的中低温酸性流体。
It is concluded that the fluid forming this type of copper-gold deposit is one high oxygen and sulphur fugacity and low-to-moderate temperature acid fluid.
认为形成这一类型矿床的流体是一种高氧逸度、高硫逸度的中低温酸性流体。
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