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图林斯克铜矿开采瓦季姆-亚历山德罗夫矿床已有二百二十五年的历史。矿体通常赋存于矽卡岩与石灰岩的接触带内,为透镜状、管状和层状,倾角75°～90°。矿体尺寸的变化很大,沿走向10～300米,沿倾斜10～400米,厚度为2～60米。地表没有露头,矿体上部在地表以下100多米处尖灭。围岩为矽卡岩(f=10～12)、石灰岩(f=6～8)和钠长斑岩(f=10～12)。采矿方法主要为分段平巷崩矿的阶段矿房法。用阶段强制崩落法开采了有数百万吨
The Tłinsk Copper Mine has been mining the Vadim-Alexandrov deposit for two hundred and twenty-five years. The ore body usually occurs in the contact zone between skarn and limestone, which is lenticular, tubular and layered with the inclination of 75 ° ~ 90 °. Large changes in ore body size, along the direction of 10 to 300 meters, along the slope of 10 to 400 meters, a thickness of 2 to 60 meters. No outcrops on the surface, the upper part of the ore body at the surface below 100 meters sharp end. Surrounding rocks are skarn (f = 10-12), limestone (f = 6-8) and albite (f = 10-12). The mining method is mainly for the stage of mine roof collapse method. Millions of tons have been mined by stage forced caving