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斑岩型矿床是一种重要的金属矿床类型,为世界上提供了57%的铜资源和9%的金资源(Singer et al.,2005)。从全球范围来看,浅成热液型和斑岩型金铜矿床在时空上与侵入岩浆作用有关(Jégo Stébastien et al.,2012),岩浆和热液过程的共同作用形成了此类矿床。元素在流体和熔体间交换、分配过程是岩浆热液矿床形成的重要环节。研究金在硅酸盐熔体和流体中的分配行为及其影响因素对认识中酸性岩浆演化与成矿的关系具有重要意义。关于金在花岗质流体/
Porphyry deposits are an important type of metal deposit providing the world with 57% copper and 9% gold (Singer et al., 2005). Globally, epithermal and porphyry gold-copper deposits are associated with intrusion of magmatic rocks in time and space (Jégo Stébastien et al., 2012). The magmatic and hydrothermal processes together form these deposits . Elements in the fluid and melt exchange, the distribution process is an important part of the formation of magmatic hydrothermal deposits. The distributive behavior of research grants in silicate melts and fluids and their influencing factors are of great significance for understanding the relationship between acid magmatic evolution and mineralization. About Gold in Granitic Fluid /