秦岭造山带是我国重要的成矿带。其中凤太矿集区位于南秦岭造山带,是秦岭多金属成矿带的重要组成部分。文章简述了凤太矿集区地层、构造、岩浆岩等方面的地质背景,结合双王金矿、八卦庙金矿和铅硐山-东塘子铅锌矿等已知典型矿床地质特征,从而分析区域成矿潜力,为找矿提供一定参考意义。 Qinling orogenic belt is an important metallogenic belt in China. The Fengtai ore district is located in the South Qinling orogen and is an important part of the Qinling polymetallic metallogenic belt. In this paper, the geological background of strata, structure and magmatic rocks in Fengtai ore district are briefly described. Combined with the geological characteristics of known typical deposits such as Shuangwang gold deposit, Baguimiao gold deposit and Lead Mountain - Dongtangzi lead-zinc mine, Therefore, the regional metallogenic potential can be analyzed to provide a reference for prospecting.