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Publikováno v:
Georesursy, Vol 23, Iss 1, Pp 85-93 (2021)
The article describes the geological structure of the Sokolovsk and Krasnokamensk massifs located in the central part of the Western subzone of the Chelyabinsk-Adamovka zone of the Southern Urals. They are of Lower Carboniferous age and break through