FEATURES OF THE GEOLOGICAL STRUCTURE OF THE VAUDIL BROWN COAL DEPOSIT

Geochemistry carbonate metamorphism terrigenous deposits limestone alleurolite slate marl dolomite structural floor pre-Mesozoic orumentum retinue suite of acglomerates sandstones tier

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This article briefly describes the hological structure of the Vaudil site located on the territory of the Fergana region, and the main emphasis is placed on the composition of the coal seams located on the site, what rocks are4 associated with them and how distributed they are.