The gold deposit is a postmagmatic mesothermal-epithermal quartz-vein type gold deposit.
该矿床属岩浆期后中一低温热液充填一交代石英脉型金矿床。
The gold deposit is a postmagmatic mesothermal-epithermal quartz-vein type gold deposit.
该矿床属岩浆期后中一低温热液充填一交代石英脉型金矿床。
It used to be considered that the wolframite_quartz veins in Xihuashan orefield has been crystallized from hyperthermal or mesothermal solution.
过去一直认西华山黑钨矿石英脉是高中温热液充填而成。
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