geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3472Research ArticleНаучные сообщенияShort communicationsФормирование рельефа проградационного шельфа Таманского полуостроваRelief formation of the programming shelf of the Taman peninsularПавлидисЮ. А.PavlidisYu. A.ЩербаковФ. А.ShcherbakovF. A.Институт океанологии им. П.П. Ширшова РАНРоссия199814122023019199Copyright © Павлидис Ю.А., Щербаков Ф.А., 20232023Павлидис Ю.А., Щербаков Ф.А.Pavlidis Y.A., Shcherbakov F.A.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://geomorphology.igras.ru/jour/article/view/3472

The structure and origin of the outer part of Taman peninsular programming shelf are analyzed. This sedimentary prismatic body was formed due to alluvial and deltaic accumulation in periods of the pleistocene transgression.

The structure and origin of the outer part of Taman peninsular programming shelf are analyzed. This sedimentary prismatic body was formed due to alluvial and deltaic accumulation in periods of the pleistocene transgression.

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The authors declare that there are no conflicts of interest present.