Articles | Volume 11, issue 6
https://doi.org/10.5194/se-11-2047-2020
https://doi.org/10.5194/se-11-2047-2020
Research article
 | 
10 Nov 2020
Research article |  | 10 Nov 2020

Lithological and geomorphological indicators of glacial genesis in the upper Quaternary strata, Nadym River basin, Western Siberia

Oleg Sizov, Anna Volvakh, Anatoly Molodkov, Andrey Vishnevskiy, Andrey Soromotin, and Evgeny Abakumov

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Cited articles

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Andreev, Y. F.: About the relationship of linear-ridge topography with tectonic structures in the north of Western Siberia (in the field of permafrost development) Geologiya i geokhimiya, Geol. Geochem., 3, 76–94, 1960. 
Astakhov, V. and Nazarov, D.: Correlation of Upper Pleistocene sediments in northern West Siberia, Quaternary Sci. Rev., 29, 3615–3629, 2010. 
Astakhov, V., Shkatova, V., Zastrozhnov, A., and Chuyko, M.: Glacio-morphological Map of the Russian Federation, Quaternary Int., 420, 4–14, 2016. 
Astakhov, V. I.: On chronostratigraphic units of the Upper Pleistocene in Siberia, Geol. Geofiz., 47, 1207–1220, 2006. 
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Short summary
Analysing the genesis of Quaternary sediments is important for understanding the glaciation history and development of marine sediments in the northern part of Western Siberia. The key features of sedimentation and landform formation have been characterised for the first time in an example of a lithological column from the lower sources of the Nadym River. A comprehensive analysis was performed on the lithological, petrographic and geomorphological data from the upper Quaternary stratum.