Yu. Kozlenko
Institute of Geophysics of NAS of Ukraine, Kyiv
PALEOSTRUCTURAL RECONSTRUCTION OF THE SEDIMENTARY BASIN IN THE NW BLACK SEA IN MEZO-CЕNOZOIC
Sequential examination of Scythian Plate structure via backsripping methods is allowed to substract numerous dislocations at the Earth crust, most of which had originated over the surface of cemented platform at the stage of sedimentary cover deposit. According to the obtained data the Black Sea bed actual morphology is controlled by Mesozoic deep faults. It is found that in the course of time the tectonic activity of Scythian Plate was becaming consistently extinct.
Key words: paleostructural reconstruction, paleostructural sequence, NorthWest shelf of the Black Sea, Carkinit downfold, Calamit swell, Marginal step.
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