Abstract:The accomplished analysis has found out that the study basins were the parts of the Black Sea-Caspian basin system in the Mesozoic era, partly participated in dislocation tectonics later on, and are the part of the Alpine folding zone from the viewpoint of the modern tectonic zoning. Furthermore, the analysis has set the main stages of the sedimentation cross-section formation with the specified sedimentary depocenters at each stage, which allows reconstructing the sedimentation evolution. The studies of the d… Show more
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