Abstract: The paper discussed primarily the mineralization features of Qiangma gold deposit, it suggested that the formation of the gold deposit have much to do with late Yan shanian magmatic activity, Taihua group metarnophic strata, the deposit is of mesothermal genetic type. The occurren ces of auriferous quartz veins, the scale and spaticl Localization of industrial ore bodies are strictly controlled by fractures, it provides evidence for production and progressive eploration works in the mining district.