geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2873Research ArticleНаучные сообщенияShort communicationsПриазовско-Донецкая возвышенность гетерогенная кайнозойская морфоструктураThe Azov-Donets Upland - a heterogeneous Cenozoic morphostructureГофштейнИ. Д.HofsteinL. D.Институт геологии и геохимии горючих ископаемых АН УССРУкраина19911912202201Геоморфология5659Copyright © Гофштейн И.Д., 20222022Гофштейн И.Д.Hofstein l.D.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/2873

In spite of the structural difference between the Donets Ridge and the Azov crystalline massif as well as different history of their formation, they form a single upland without marked division. Paleogeographic data corroborate this thesis: an upland within the same limits existed throughout the whole Cenozoic time. The unity composed of the Donets Ridge and the Azov massif has not been broken in spite of epeirogenic movements.

In spite of the structural difference between the Donets Ridge and the Azov crystalline massif as well as different history of their formation, they form a single upland without marked division. Paleogeographic data corroborate this thesis: an upland within the same limits existed throughout the whole Cenozoic time. The unity composed of the Donets Ridge and the Azov massif has not been broken in spite of epeirogenic movements.

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