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大渡河金成矿带是20世纪80年代以来西南地区发现的一个重要金成矿集中区,金矿床主要分布在前震旦系康定杂岩中。三碉金矿床分布于大渡河成矿带北部,海拔2800~3000 m。目前对该矿床矿石特征的研究较低,故开展矿石特征的研究,对该矿床成因及指导三碉金矿床下一步地质找矿勘探具
The Daduhe gold metallogenic belt was an important gold mineralization concentrated area discovered in Southwest China since the 1980s. The gold deposits are mainly distributed in the former Sinian Kangding complex. Sanda gold deposits located in the northern Dadu metallogenic belt, elevation 2800 ~ 3000 m. At present, the research on ore features of this deposit is relatively low, so it is necessary to carry out the research on the characteristics of the ore and to study the genesis of the deposit and guide the prospecting tools for the next step of the Getao gold deposit