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胡村矿床是我国长江中下游多金属成矿带铜陵矿集区狮子山矿田中的一个大型层控矽卡岩型—斑岩型铜矿,近年来深部勘探工程又在原有胡村铜矿床基础上新发现了深部岩体中发育的钼矿床。然而,对于该矿床中深部“层状硫化物”的成矿物质来源和成因机制至今仍存在争议,主要有燕山期岩浆热液成因(常印佛等,1991;毛
Hucun deposit is a large stratified skarn-porphyry type copper deposit in the Shizishan ore-field in the area of the Tongling Ore Concentration Zone, the polymetallic metallogenic belt in the middle and lower reaches of the Yangtze River. In recent years, the deep exploration project has been carried out in the Hucun copper deposit On the basis of newly discovered molybdenum deposit developed in deep rock mass. However, there are still controversies about the sources and genesis of the ore-forming materials in the deep “stratiform sulphides ” in this deposit, mainly due to the genesis of the Yanshanian magmatic hydrothermal fluids