Abstract

The evolution of views of the stratigraphy of Berriasian–Lower Aptian deposits of West Siberia is described. In connection with a clinoform model of the section structure, suggestions are made for its stratification; according to new recommendations to the stratigraphic scheme, paleogeographic reconstructions were carried out for the four stratigraphic units identified in the Berriasian–Early Aptian play.

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