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doi: 10.24412/2687-1092-2023-10-299-309
Institute of the Earth's Cryosphere, Tyumen Scientific Center SB RAS, Tyumen, Russia
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Abstract. Data on the paleocryological development of the north of the West Siberian Lowland in the Quaternary are summarized. Information on the region has become contradictory, and to resolve the contradictions, methodological approaches are required that can increase the likelihood of recognition and verification of past phenomena. The basis of such approaches is their implementation based on the principle of actualism: the range of modern manifestations of the cold world is wide, there is reliable parametric information on them, and it is this that allows for reliable comparisons of the processes of the present and the past using the method of comparative analogy. On this basis, representative reconstructions were carried out, and it was established that the development of the region in the Quaternary took place under conditions in which the existence of hyperarid cold deserts and ice sheets was unrealistic, but cryogenic processes of various types were actively occurring. Keywords: Western Siberia, Pleistocene, glacial phenomena, cryogenesis
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Cite this article:
Sheinkman V.S., Sedov S.N. Glacial-free development of the West Siberian north of and phases of epicryogenesis, syncryogenesis and postcryogenesis // Relief and Quaternary deposits of the Arctic, Subarctic and North-West Russia. 2023. Issue 10. P. 299-309. doi: 10.24412/2687-1092-2023-10-299-309
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