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卡兰古铅矿地处以塑性变形为主的奇自拉夫背斜的卡拉古次级褶皱,为一套碳酸盐岩夹碎屑岩建造。矿化受这两组褶皱构造的控制,分南、北两个矿带,以北矿带为主。赋存在卡拉巴西塔克组(C1kl)第一、第二、第三岩性段灰黑色白云岩化灰岩、灰白色厚层碎裂状白云岩中。矿床成因类型为密西西比河谷型-碳酸盐岩型。
The Kalang Galena is located in the Karakuk subfold of the Chiracra anticline, dominated by plastic deformation, and is constructed from a suite of carbonate clastic rocks. By the control of the two sets of fold structure, mineralization is divided into two ore zones in the south and the north, mainly in the northern ore zone. It is found in the first, the second and the third lithology dolomite limestone in the Tachai Formation (C1k1) of Calabac, and in the thick gray-bedded dolomite. The genetic type of the deposit is the Mississippi Valley-Carbonate type.