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白牛厂银铅锌硫化物矿体赋存在中寒武统海相细碎屑岩中，白垩纪花岗岩体接触带附近。矿床的形成经历了中寒武世海底喷溢沉积成矿作用和燕山期酸性岩浆热液叠加成矿作用，具多源、多成因和多旋回演化的特点，兼有外生和内生矿床的特征，是我国极具特色的细碎屑岩建造中Ｓｅｄｅｘ型矿床。
The White Cattle silver-lead-zinc sulfide orebodies occur in the Middle Cambrian marine metamorphic rocks, near the contact zone of the Cretaceous granite bodies. The formation of the ore deposit underwent the process of mid-Cambrian seabed erosional sedimentary mineralization and acid magmatic hydrothermal superposition mineralization in the Yanshanian period, with multi-source, multi-genesis and multi-cycle evolution characteristics, with both exogenous and endogenous mineral deposits Features, is China’s unique characteristics of finely divided rocks Sedex deposit.