斑岩铜矿床 meaning in Chinese

porphyry copper deposit

Generally magmatic hydrothermal cu and au deposits enrich cl and s , but w and sn deposits are rich f systems . in this paper , in order to study the relationship between the cu , w and
本文以著名的江西德兴铜厂超大型斑岩铜矿床和大吉山钨矿床作为研究对象，研究f 、 cl与w 、 cu成矿的关系。
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。