M.V. Kozlenko
Institute of Geophysics of NAS of Ukraine, Kyiv
SEDIMENTATION RATE AS AN INDICATOR OF THE TECTONIC PROCESSES ON THE NW BLACK SEA SHELF
According to common-depth-point shooting data along the profile 568 408, sediment accumulation rates in central part of the Black Sea North-West shelf are estimated over six time cuts, from middle Jurassic to present. Obtained diagrams showed sedimentation unstability through time and along the profile. Based on curve bend points analysis the faults are indicated; some of them may be the source of hydrocarbon income. On the basis of analysis of sedimentation dynamic and its local maximums migration, the scheme of Scythian Plate evolution in Meso-Cenosoic along the profile is suggested.
Key words: the Black Sea NorthWest shelf, sediment accumulation rates, faults, Scythian Plate evolution, Meso-Cenosoic.
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