geomorfГеоморфология и палеогеографияGeomorfologiya i Paleogeografiya2949-17892949-1797geomorf-2623Research ArticleНаучные сообщенияShort communicationsОтражение новейших структур в рельефе севера Западно-Сибирской равниныNeotectonic structures as reflected in topography of north West Siberia plainСергиенкоВ. М.SergienkoA. M.БиджиевР. А.BidjievR. A.ПГО «Аэрология»Russian Federation19860911202202Геоморфология9298Copyright © Сергиенко В.М., Биджиев Р.А., 20222022Сергиенко В.М., Биджиев Р.А.Sergienko A.M., Bidjiev R.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/2623

Some results are presented of the work on the Gydan and Taz peninsulas aimed to identification of local uplifts within the Quaternary marine sediments. The uplifts are proved to be directly connected with positive present-day landforms and mostly inherited from Mesozoic local structures, the latter containing deposits of gas and condensate. The data presented had been obtained during the geological survey of the area using both space images and aerial photoes of various scales.

Some results are presented of the work on the Gydan and Taz peninsulas aimed to identification of local uplifts within the Quaternary marine sediments. The uplifts are proved to be directly connected with positive present-day landforms and mostly inherited from Mesozoic local structures, the latter containing deposits of gas and condensate. The data presented had been obtained during the geological survey of the area using both space images and aerial photoes of various scales.

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