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矿区位于海拔标高1200～2200公尺的乌多坎山脉的中部。强烈的大陆性气候。终年冻土至少延深500毫米。从成因上说,乌多康铜矿体是因沉积而出现的含铜砂岩矿床。根据铜矿物的氧化程度,矿石分为三种类型:硫化矿、混合矿及氧化矿。按照矿物组成,硫化矿分为斑铜矿-辉铜矿和黄铜矿。在斑铜矿-辉铜矿中可选出主要的斑铜矿和主要的辉铜矿。黄铜矿具有强烈的依附性质;因黄铁矿和黄铜矿共生。
The mine is located in the middle of the Udo-Kundan Range at 1200 ~ 2200 meters above sea level. Strong continental climate. Permafrost throughout the year at least 500 mm deeper. From a genetic point of view, the Udokang copper ore body is a deposit of copper-bearing sandstone. According to the degree of oxidation of copper minerals, the ore is divided into three types: sulfide ore, mixed ore and oxide ore. According to the mineral composition, sulphide ore is divided into the bornite-chalcopyrite and chalcopyrite. The major beryllitites and major chalcocides are selected in the bornite-chalcocite. Chalcopyrite has a strong dependency; pyrite and chalcopyrite symbiosis.