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古谢沃戈尔钛磁铁矿床的主要矿物是辉岩,其次是辉长岩、苦闪橄榄岩、叶碲铋矿、角闪岩和脉石。工业矿化是在辉岩、叶碲铋矿中的钛磁铁矿和钛铁矿浸染,以及在橄榄辉岩中较少的浸染。按其构造特点和物理力学性质,矿石的非均质性导致矿石颗粒和集合体的尺寸变化范围很大。往往沿一个生产水平延续1.5～2km 的作业线,其矿岩的可钻性和可爆性却相差20～30倍之多。在这样
The main minerals of the ancient Svogor titanomagnetite deposit are pyroxene, followed by gabbro, maser peridotite, telluride bismuth ore, amphibolite and gangue. Industrial mineralization is the dissemination of titanomagnetite and ilmenite in pyroxene and telluride bismuth and the less dip in olivine. According to its structural characteristics and physical and mechanical properties, ore heterogeneity leads to a large range of sizes of ore particles and aggregates. Often along a production level of 1.5 ~ 2km extension of the line, the drillability of mine rock and blastability but a difference of 20 to 30 times. In this way