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卡依斯克矿由许多储藏量大的急倾斜矿体所组成。它的深层矿带由夹层、辉绿玢岩、层状凝灰岩的透镜状矿体构成,矿体有大量明显的构造裂隙和软弱带,且片理发育。此外,各种形式的绢云母片岩可产生片落和隆起现象。矿体开采的第一阶段,由于顶盘很厚,富矿埋藏深,致使采矿工作延缓11～12年。为了缩短回采储量极大的名为富矿体的期限,采用露天和地下同在一个垂直而上进行开采的联合采矿法。露天与地下采场之间留下100米高的矿柱,这个矿柱开始时期为矿石柱,以后用人工矿
Kalisike mine is composed of many large reserves of steep ore body. Its deep ore belt is composed of lenticular, diabase pluton and lenticular tuffite lenticular ore body. The ore body has a large number of obvious structural fractures and weak belts, and the development of the belt. In addition, various forms of sericite schist can produce patchwork and uplift. The first phase of ore body mining, due to the thick top plate, deep burial rich ore, resulting in mining delays 11 to 12 years. In order to shorten the period of recovery of so-called rich ore bodies, a combination of open pit and underground mining is adopted in a vertical mining operation. Open pit and underground stope left between the 100-meter high ore pillar, the pillar of the ore pillar at the beginning, after the artificial mine