摘要
黄山南矿区经过多年的生产及勘探工作,揭露矿石的类型及矿体产状较前期的认识有了较大的变化。矿床成因复杂,认为该矿区成矿过程经历了超基性岩熔离矿化期—构造挤压拉伸变形期—酸性花岗岩熔蚀改造期—岩浆期后热液富集、构造压扭变形就位期。矿床成因并不是单一的超基性熔离矿床,应为超基性岩熔离改造型铜镍矿床,并根据矿床的成因,分析该矿区的控矿因素。
After many years of production and exploration work,Huangshan Nan Southern mining area has revealed great changes in ore types and ore occurrences.The genesis of the ore deposit is complex,and it is considered that the metallogenic process of this mining area has experienced the period of ultrabasic lava mineralization-tectonic extrusion stretch deformation period-acid granite remelting period-post magmatic hydrothermal enrichment and tectonic compression and deformation.The genesis of the deposit is not a single ultrabasic deposit.It should be a copper nickel and cobalt deposit formed by the modification of the ultrabasic rock,and the ore controlling factors are analyzed in accordance with the genesis of the deposit.Through the new understanding of ore genesis and ore controlling factors,it has important guiding significance for subsequent geological prospecting and production prospecting.
引文
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