造山型金矿为世界上最重要的金矿类型,被认为是变质流体成矿的典型代表(Goldfarb et al.,2005)。此外,变质地体中部分贱金属矿床(Cu、Pb、Zn)具有与造山型金矿类似的地质和地球化学特征,也被认为形成于变质流体(如Leach et al.,1998;Zhong et al.,2012,2013),部分学者亦将其命名为造山型矿床(陈衍景,2006)。目前 The orogenic gold is the most important type of gold deposit in the world and is considered as a typical representative of metamorphic fluid mineralization (Goldfarb et al., 2005). In addition, some of the basement metal deposits (Cu, Pb, Zn) in the metamorphic terrain have similar geological and geochemical characteristics as orogenic gold deposits and are also considered to be formed in metamorphic fluids (eg Leach et al., 1998; Zhong et al ., 2012,2013), some scholars also named it orogenic type deposit (Chen Yanjing, 2006). Currently