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- W117911986 abstract "The major geological and paleoecological events of the Late Pleistocene in the north of West Siberia are two glaciations {Yermak (Zyryan) and Sartan} and three transgressions (Kazantsev, Kargin and post-glacial) (Arkhipov, 2000) (Fig. 3.1). As stated above, the Kazantsev transgression is correlated with the Eemian transgression of West Europe and MIS 5e (Troitsky, 1966; Gudina, 1976; Arkhipov, 1997, 2000). The Kazantsev Horizon lies on erosional surface of the Sanchug marine sequence and the Tazov moraine (Troitsky, 1969). It is composed of alternating sand, silt and clays (40–50 m) (Arkhipov et al., 1992)." @default.
- W117911986 created "2016-06-24" @default.
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- W117911986 date "2009-01-01" @default.
- W117911986 modified "2023-09-26" @default.
- W117911986 title "Main Geologic-Paleoecological Events of the Late Pleistocene in the North of Western Siberia" @default.
- W117911986 doi "https://doi.org/10.1007/978-3-642-00288-5_3" @default.
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