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屏峰矿区是一个以硫为主的大型多金属矿床,铅、锌亦可达中型规模,并伴生有铂、金等元素。矿体产生于沉积岩夹火山岩中,含矿三层,矿体产状同围岩一致,其形态呈层状和似层状。矿区内构造有华夏系和新华夏系断裂,控制了矿体的分布。岩浆活动频繁,并伴有矿液活动,使沉积形成的矿体更趋富集。根据矿体中出现大量的铂元素,推测矿区内存在属裂谷成因的古火山岩——基性和超基性岩体,为找铂提供了新的线索.
Pingfeng mine is a sulfur-based large-scale polymetallic deposits, lead, zinc can reach the medium-sized scale, accompanied by platinum, gold and other elements. Ore bodies are formed in sedimentary rock-lava volcanic rocks and contain three layers of ore. The ore body is consistent with the surrounding rock and has a layered and layered form. There are Huaxia and Neo-Huaxia faults in the mining area, which control the ore body distribution. The magmatic activity is frequent and accompanied by the activity of mineral fluid, enriching the ore body formed by sedimentation. According to the presence of a large number of platinum elements in the ore bodies, it is speculated that there are ancient volcanic rocks that belong to rift origin in the mining area - basic and ultrabasic rocks, which provide new clues for platinum prospecting.