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野外和室内研究表明,武山铜矿床为大陆地壳断裂拗陷带中形成的块状硫化物矿床。其成因与中石炭世海相火山作用有关。与主矿层伴生的武山英安质晶屑熔岩的裂变径迹年龄为345±37m.y.。块状硫化物矿床按成矿地壳背景可分成三种类型:大洋地壳上形成的塞浦路斯型;过渡性地壳上形成的黑矿型和大陆地壳上形成的华南型。华南型与塞浦路斯型和黑矿型在地质特征上有着显著的差别。
Field and laboratory studies show that the Wushan copper deposit is a massive sulphide deposit formed in the continental crust depression and depression zone. Its causes are related to the marine volcanism in the middle Carboniferous. The fission track age of the Wushan Yingan crystalline cuttings associated with the main ore is 345 ± 37m.y. According to the background of metallogenic crust, the massive sulfide deposits can be divided into three types: the Cyprus type formed on the oceanic crust; the South China type formed on the black ore type formed on the transitional crust and the continental crust. South China type and Cyprus type and type of black ore in the geological characteristics of a significant difference.