Abstract

The mineralized zones of the Zengibobo-Sheikhjelinskaya area are timed to narrow violations of the tectonic zones of the north-eastern and north-western direction. The main form of gold-containing mineralization are small sharp-falling veins and lenses of quartz containing interspersed pyrite, arsenopyrite, chalcopyrite and pyrrotin, which are represented by gold-quartz, gold-arsenopyrite-pyrite natural type of ores.

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