Structure and the formation of the carbonate strata in the salt formation of the Northern zone of the border projections in the Pripyat trough
It is shown that the carbonate strata in clay-halite subformation of the Nothern zone of the border projections in the Pripyat trough was created as a result of erosion of intrasalt deposits in the North-Pripyat shoulder and their deposition in border part of the salt basin.