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Seismic geomorphological analysis of the oligocene-neogene sediments in the north-eastern part of the Black Sea

https://doi.org/10.33623/0579-9406-2021-4-38-51

Abstract

The evolution of the deep-sea sedimentation system in the north-eastern part of the Black Sea during the Oligocene-Pliocene is considered mainly on the basis of seismic data. The fans and erosion canyons formation time is presumably related to the regressive-transgressive stages in the history of the Eastern Paratethys. The source areas of detrital sediments in the Tuapse Trough are identified. The sedimentation model of the Tuapse Trough and the changes in the Trough’s morphology since the Oligocene were reconstructed based on the analysis of the thickness maps and the onlap surfaces on the northern side of the Shatsky Swell. Paleogeographic maps were compiled for the Late Oligocene-Early Miocene (Maikop), Middle Miocene, and Pliocene.

About the Authors

G. V. Baskakova
LLC «RN-Exploration»
Russian Federation

121151, Moscow, Mozhaisky Val, 8



N. A. Kulyukina
LLC «RN-Exploration»
Russian Federation

121151, Moscow, Mozhaisky Val, 8



T. A. Arzamastseva
LLC «RN-Exploration»
Russian Federation

121151, Moscow, Mozhaisky Val, 8



N. A. Malyashev
Rosneft Oil Company
Russian Federation

117997, Moscow, Sofiyskaya Embankment, 26/1



O. A. Almendinger
LLC «RN-Exploration»
Russian Federation

121151, Moscow, Mozhaisky Val, 8



A. M. Nikishin
Lomonosov Moscow State University
Russian Federation

119991, Moscow, GSP-1, Leninskiye Gory, 1



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For citations:


Baskakova G.V., Kulyukina N.A., Arzamastseva T.A., Malyashev N.A., Almendinger O.A., Nikishin A.M. Seismic geomorphological analysis of the oligocene-neogene sediments in the north-eastern part of the Black Sea. Moscow University Bulletin. Series 4. Geology. 2021;1(4):38-51. (In Russ.) https://doi.org/10.33623/0579-9406-2021-4-38-51

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