geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2063Research ArticleНаучные сообщенияShort communicationsГеоморфолого-геокриологическое строение восточносибирского сектора Арктического шельфа и его развитие в позднем плейстоцене-голоценеGeomorphologic and geocryologic features of the East-Siberian sector of the Arctic shelf and its development in the Late Pleistocene - HoloceneДаниловИ. Д.DanilovI. D.ВласенкоА. Ю.VlasenkoA. Ju.БирюковВ. Ю.BiryukovV. Yu.Московский государственный университет имени М.В.Ломоносова, Геологический факультетРоссияНПП "Эколого-аналитический центр"Россия20011507202201Геоморфология4553Copyright © Данилов И.Д., Власенко А.Ю., Бирюков В.Ю., 20222022Данилов И.Д., Власенко А.Ю., Бирюков В.Ю.Danilov I.D., Vlasenko A.J., Biryukov V.Y.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/2063

Analysis of the geology-geomorphologic data allowed us to create a model of coasal-shelf cryolithosphere evolution in the Eastern Arctic Shelf of Eurasia (the Eastern Siberian Sea as an example) during the last 80000 years. This epoch includes two large cryochrons corresponding to the Zyryan and Satan regressions, and two thermochrons corresponding to the Karga and Holocene transgressions.

Analysis of the geology-geomorphologic data allowed us to create a model of coasal-shelf cryolithosphere evolution in the Eastern Arctic Shelf of Eurasia (the Eastern Siberian Sea as an example) during the last 80000 years. This epoch includes two large cryochrons corresponding to the Zyryan and Satan regressions, and two thermochrons corresponding to the Karga and Holocene transgressions.

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