geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-3213Research ArticleНаучные сообщенияShort communicationsРельеф юго-восточного Призайсанья и некоторые особенности четвертичного осадконакопленияRelief of the area south-east of the Zaisan Lake and some characteristics of the Quaternary sedimentationУслугинМ. О.UsluginM. O.ХворовБ. И.KhvorovB. I.КоротушенкоЮ. Г.KorotushenkoYu. G.БоднарС. П.BodnarS. P.Алтайская геолого-геофизическая экспедиция, г. Усть-КаменогорскРоссия1995100320230393101Copyright © Услугин М.О., Хворов Б.И., Коротушенко Ю.Г., Боднар С.П., 20232023Услугин М.О., Хворов Б.И., Коротушенко Ю.Г., Боднар С.П.Uslugin M.O., Khvorov B.I., Korotushenko Y.G., Bodnar S.P.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/3213

Four stages are distinguished in the relief development in the Zaisan Lake basin, each of them being associated with a complex of built-up surfaces: 1) glacial-fluvioglacial-lacustrine stage ( Kiinzhirian) - the end of the Middle Pleistocene; 2) glacial-alluvial - lacustrine (Katonian) - beginning of the Late Pleistocene; 3) lacustrine-alluvial stage (post-glacial) - the end of the Late Pleistocene; 4) alluvial - the Holocene. Geomorphic structure and the Quaternary sediments distribution suggest general upwarping of the area during the Quaternary, the movement amplitudes decreasing gradually.

Four stages are distinguished in the relief development in the Zaisan Lake basin, each of them being associated with a complex of built-up surfaces: 1) glacial-fluvioglacial-lacustrine stage ( Kiinzhirian) - the end of the Middle Pleistocene; 2) glacial-alluvial - lacustrine (Katonian) - beginning of the Late Pleistocene; 3) lacustrine-alluvial stage (post-glacial) - the end of the Late Pleistocene; 4) alluvial - the Holocene. Geomorphic structure and the Quaternary sediments distribution suggest general upwarping of the area during the Quaternary, the movement amplitudes decreasing gradually.

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