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２８０１铜铀金矿化点位于康滇地轴南段。受ＳＮ向罗茨－易门断裂和元谋绿汁江断裂所控制。矿化产于旁侧的次级断裂交叉部位。含矿断裂为因民组与美党组之间的不整合面层间构造断裂破碎带。近矿围岩为含碳千枚岩，赋矿岩石为构造角砾岩。矿石矿物成分复杂，有沥青铀矿、黄铜矿、黄铁矿、辉钼矿等，近矿围岩蚀变发育，主要有钠长石化、白云石化、硅化、硫化物化、水云母化、赤铁矿化等。成矿时代为７２９Ｍａ，成矿温度Ｔ／Ｋ为５７３．１５～６７３．１５，属沉积变质－热液改造型矿化，具有不整合脉型和碱交代型双重特征。
2801 copper uranium gold mineralization point is located in the southern section of the axis of health and Yunnan. Controlled by SN to Roots-easy-door fault and Yuanmou-green Jujiang fault. Mineralization occurred in the side of the secondary fracture intersection. The ore-bearing fault is the fault zone formed by the unconformity between the Yinmin and the Udonist formations. The ore-bearing rocks are carbonaceous phyllites and the ore-bearing rocks are structural breccias. Ore mineral composition is complex, with bitumen uranium, chalcopyrite, pyrite, molybdenite, near the ore rock alteration development, there are albite, dolomitization, silicification, sulfide, mica, red Iron ore and so on. The mineralization age is 729Ma, and the metallogenetic temperature T / K is 573.15 ~ 673.15. It belongs to the metamorphism-hydrothermal mineralization with dual characteristics of unconformity vein type and alkali metasomatism.