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矿区位于腾冲西北部东河铁、铜、铅锌多金属成矿区,区内早白垩世花岗岩浆活动强烈,矽卡岩型矿床发育,形成众多铁、铜、铅、锌矽卡岩型矿床,是腾冲西北部重要成矿区,棋盘石矽卡岩型铅锌矿即是其中之一。矿床形成与早白垩世中酸性花岗岩关系密切,矿体位于上二叠统碳酸盐岩外接触带矽卡岩中。地层、岩体对矽卡岩及矿体的控制作用明显。
The ore district is located in the Donghe iron, copper and lead-zinc polymetallic metallogenic area in the northwest of Tengchong. The Early Cretaceous granite magmatism was strongly active in the area, with skarn deposits developing, forming many iron, copper, lead and zinc skarn deposits, Is an important metallogenic area in the northwest of Tengchong, which is one of the chessboard skarn-type lead-zinc deposits. The mineralization is closely related to the Early Cretaceous acidic granite. The ore body is located in the outer contact zone skarn of the Upper Permian carbonate. Strata, rock mass on the skarn and ore control effect is obvious.