Interactions of Paleocryogenic, Pedological and Archeological Processes as a Factor of the Formation of Complex Archeological Site Bolshoi Salym 4 (Middle Taiga, Western Siberia)-Reference-Cited by-同舟云学术

Interactions of Paleocryogenic, Pedological and Archeological Processes as a Factor of the Formation of Complex Archeological Site Bolshoi Salym 4 (Middle Taiga, Western Siberia)

Published:2024 Issue: Volume: Page:211-213
ISSN:2522-8714
Container-title:Advances in Science, Technology & Innovation
language:en
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Author:

Kurasova Alina,Balueva Yulia,Konovalenko Maria,Konstantinov Alexandr,Loiko Sergey,Novoselov Andrey,Kulizhskiy Sergey

Publisher

Springer Nature Switzerland

Link

https://link.springer.com/content/pdf/10.1007/978-3-031-48754-5_49

Reference8 articles.

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2. Konovalenko, M. V., Balueva, Y. V., Serikov, Y. B. (2017). Bolshoi Salym 4—a new mesolithic site in the North of Western Siberia (the first results of the study). Stratum plus. 1, pp. 201–218. (in Russian).

3. Varlamov, I. P., et al. (1972). Geomorphology of the West Siberian plain (Explanatory note to the geomorphological map of the West Siberian Plain, scale 1:500,000), Tr. SNIIGGIMS. 134 (in Russian).

4. Scientific-Applied Handbook on Climate of the USSR. (1998). Ser. 3: Long-Term Data, Parts 1–6, No. 17: Tyumen and Omsk Oblasts. Gidrometeoizdat (in Russian).

5. Garankina, E. V., Lobkov, V. A., Shorkunov, I. G. & Belyaev, V. R. (2022). Identifying relict periglacial features in watershed landscape and deposits of Borisoglebsk Upland, Central European Russia. Journal of the Geological Society 179(5), jgs2021–135. https://doi.org/10.1144/jgs2021-135.