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矿床赋存于北——西走向的大向斜层的一翼,倾角45°,有厚度与走向不同的三个平行矿体。上部矿体厚12米,走向长1800米;中间矿体厚18米,走向长2000米;第三矿体厚20米,走向长2700米。矿体夹层为废石或贫矿厚17米,三个矿体在走向的中部约1000米处汇合,作为一个矿体开采,总厚度约为60米。矿体在厚度与走向上都是稳定的。矿物为斑铜矿、黄铜矿、辉铜矿,以浸染状及细脉状存在,横切矿体走向。有时遇到孔雀石、赤铜矿,蓝铜矿、硅孔雀石和自然铜。可以清楚看到层理和解理面。距地表以下300米有二次富
The deposit occurs in a wing of the syncline north-west strike with an inclination of 45 ° and three parallel ore bodies with different thickness and strike. The upper part of the ore body is 12 meters thick and is 1800 meters long. The middle ore body is 18 meters thick and extends to 2000 meters long. The third ore body is 20 meters thick and 2700 meters long. The orebody interbed is 17 meters thick of waste rock or lean ore, and the three ore bodies converge about 1000 meters in the middle of the strike and are mined as an ore body with a total thickness of about 60 meters. Ore body thickness and direction are stable. Minerals for the adhibitites, chalcopyrite, chalcocite, with disseminated and fine veins exist, transverse cut ore. Occasionally encountered malachite, red copper, blue copper, silicon malachite and natural copper. Layers and cleavages can be clearly seen. 300 meters below the surface there are two times rich