Abstract：Shihu gold deposit in Hebei Province, belonging to pyrite sulfide type,is characterized by multistage mineralization,but the main stage of mineralization is almost coincident with the mass separation of sulfide.The sulfur in sulfide and mineralizing hydrothermal solution is derived from anatectic granitic magma.The occurrence mechanism of gold is discussed on the basis of micro-texture and crystallography.The fact that the fineness of gold in the deposit is low suggests that the development degree of sulfide has in fluenced the fineness of gold.The gold is enriched in large amounts only in the later stage of mineralization.
张步升, 王守一, 李金海. 石湖金矿矿床特征及金的赋存机理研究[J]. 地质与资源, 1997, 6(3): 183-187.
Zhang Busheng, Wang Shouyi, Li Jinhai. CHARACTERISICS OF DEPOSIT AND OCCURRENCE OF GOLD IN SHIHU GOLD DEPOSIT. GEOLOGY AND RESOURCES, 1997, 6(3): 183-187.
1997, Vol. 6 
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