Abstract
The new version of the regional stratigraphical scheme of Neogene deposits of the Ukrainian Outer Carpathians and its foreland were proposed. The results of the investigation of the planktonic microfossils allows to establish ten correlative levels, which were tacen as a basis for the correlation of prodused scheme with the International Geological Stratigraphicatime Scale. According to our investigations Neogene formations of the region are characterized by diachronous boundaries.
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