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叶尼赛山梁分布有大面积的多金属矿化作用,矿化赋存于前寒武纪固定的岩性地层层位中,因为矿化层剖面中的矿石类型与简单的矿石矿物成分相同,且矿化不受侵入岩影响,所以在研究叶尼赛山梁矿床时,研究铅-锌矿化和多金属黄铁矿化作用吋,将这种顺层的矿化做为层状矿化的代表,具有广泛的意义。众所周知,最近几年来,由于层状矿床的储量和有色金属的开采量剧增,人们对于多金属层状矿床的研究颇感兴趣,虽然出现了许多涉及到层状矿床的著作,但是关于矿
The large area of polymetallic mineralization occurs in the distribution of the Yenisayama Beam. Mineralization occurs in pre-Cambrian lithologic stratigraphic layers because the ore types in the profile of the mineralized layer are the same as the simple ore minerals. And the mineralization is not affected by intrusive rocks. Therefore, when studying the Yenisai Shanliang deposit, the study of lead-zinc mineralization and polymetallic pyrite mineralization will be based on the stratiform mineralization as stratiform mineralization Representative, has a wide range of significance. It is well-known that in recent years, due to the dramatic increase in the amount of stratiform deposits and the non-ferrous metal production, research on polymetallic stratiform deposits is of great interest. Although there have been many works related to stratiform deposit,