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塞罗德帕斯科是秘鲁中部最大的有色和贵金属矿床之一.本区的矿床与近地表的岩浆活动密切有关.塞罗德帕斯科火山岩构成由南向北延展8公里的火山锥.火山锥的产出受南北向的断裂控制.断裂附近的矿化既见于火山岩中,又见于火山锥范围以外的中生代碳酸盐岩层中.最古老的火山岩层是鲁米阿兰角砾岩,后者是由新生代以前的大量碎屑组成,胶结物是含有黑云母和斜长石的火成碎屑物质.火山锥的西部和南部,鲁米阿兰角砾岩被成分为英安
Cerro de Pasco is one of the largest colored and precious metal deposits in central Peru, and the deposits in this area are closely related to the magmatic activity near the surface. The Cerro de Pasco volcanic rock forms a volcanic cone extending 8 km north to south. The output of the volcanic cone is governed by north-south faults. The mineralization near the fault is found both in volcanic rocks and in the Mesozoic carbonate rocks beyond the volcanic cone, and the oldest volcanic rock is the Rameland breccia Is composed of a large number of detritus before the Cenozoic, cementitious material is composed of biotite plagioclase and plagioclase pyrites volcanic cone of the western and southern, Lumi Alaland breccia is composed of British security