Finally , the fluid inclusion characteristics of yinshan deposit is compared with the typical fluid - inclusion characteristics in ore formation model of porphyry copper deposit . the ore - forming fluid of yinshan deposit share certain similarities in the evolution of ore - forming fluids with porphyry copper deposits , which indicates a genetic link between the yinshan polymetallic ore deposit and porphyry copper deposit in the depth of the deposit . it is concluded that yinshan deposit is refereed to " transitional deposit " between the porphyry copper deposits and epithermal deposits 最后，将银山矿床流体包裹体特征与sillitoe提出的斑岩铜矿成矿模式进行对比得出，银山矿床的成矿流体与斑岩铜矿的成矿流体具有特征的相似性和成矿演化的继承性，认为它是一个联结深部斑岩铜矿和浅部浅成热液矿床的“过渡型矿床” ，矿床深部可能隐伏有斑岩铜矿床。
