许多研究资料都报道过造山晚期的横推断裂系统中以 H2 O- CO2 - Na Cl为主的流体与脉岩型金矿化的关系 .其中一些系统中存在晚期的低温、高盐度卤水 .这种卤水被认为是晚期分离作用的产物或作为叠加的流体导致同位素年龄再造并产生新的矿物组合 .然而 ,目前还难以建立卤水与金 Many studies have reported the relationship between H2O2-CO2-NaCl-based fluids and veins-type gold mineralization in late thrust systems of late orogeny, some of which have late-stage low-temperature and high-salinity brine. This brine is believed to be the product of late segregation or as a superimposed fluid that leads to the re-formation of isotope age and the creation of new mineral assemblages However, it is currently difficult to establish brine and gold