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造山型金矿床是指在板块汇聚边缘发生增生造山作用过程中形成的金矿床。前人研究表明,造山型金矿床的金成色一般800-950,金在造山带环境中主要以Au(HS)2-配介物形式搬运(邱正杰等,2013)。根据容矿岩石地质环境差别,造山型金矿床可分为3种主要金矿床亚类:绿岩带型、浊积岩型和Bl F型。
The orogenic gold deposits are gold deposits formed during the processes of accretionary orogeny on the edge of plate convergence. Previous studies have shown that gold formations of orogenic gold deposits generally range from 800 to 950. Gold is mainly transported in the orogenic environment as Au (HS) 2- complex (Qiu Zhengjie et al., 2013). According to the difference of geological conditions of ore-bearing rocks, the orogenic gold deposits can be divided into three major sub-types of gold deposits: greenstone belt type, turbidite type and Bl F type.