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广东省乳源一六矿田位于南岭多金属成矿带中部南缘。矿田地层为寒武系的八村群,泥盆系桂头群、东岗岭组、天子岭组和帽子峰组,石炭系孟公坳组及第四系。矿田内的构造主要为北西-北北东-近东西-近南北四组断层和褶皱轴北东向的褶皱。矿田内出露的岩体主要为燕山期的黑云母二长花岗
Guangdong Province, the source of milk 16 is located in the southern margin of Nanling polymetallic metallogenic belt. The orefields are the Eight Village Group of the Cambrian, the Guitou Group, the Donggangling Group, the Tianziling Group and the Hatzig Peak Group, the Carboniferous Menggongao Group and the Quaternary Series. The main structures in the ore field are north-east-northeast-north-north-east-northeast-east-north-north faults and fold axes. The exposed rock mass in the ore field is mainly biotite long granite in the Yanshan Period