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应用成因矿物学方法研究甘肃省西部花牛山铅锌矿床的成因，针对该矿床主矿体不同中段的３种矿石矿物进行了分析测试，认为该矿床是与γ１５侵入相关的高温热液硫化矿床，矿体的分布受断裂带的控制。
The genesis of Huabishan Pb-Zn deposit in the west of Gansu Province was studied by means of genetic mineralogy. Three ore minerals in different middle stages of the main orebody of this deposit were analyzed and tested. It is considered that the deposit is a high-temperature hydrothermal sulfide deposit associated with γ15 invasion, The orebody distribution is controlled by the fault zone.