Инд. авторы: Krivonogov S.K., Gusev V.A., Parkhomchuk E.V., Zhilich S.V.
Заглавие: Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin
Библ. ссылка: Krivonogov S.K., Gusev V.A., Parkhomchuk E.V., Zhilich S.V. Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin // Russian Geology and Geophysics. - 2018. - Vol.59. - Iss. 5. - P.541-555. - ISSN 1068-7971. - EISSN 1878-030X.
Внешние системы: DOI: 10.1016/j.rgg.2018.04.007; РИНЦ: 35520811; SCOPUS: 2-s2.0-85046633606; WoS: 000432475000007;
Реферат: eng: The Chulym and Kargat Rivers flow through chains of saucer-shaped depressions, which are swampy meadows or drainage lakes. In the past, all of them were lakes short-lived in different Holocene periods. These depressions accumulated a significant amount of the Chulym and Kargat runoff and thus influenced the water balance of Lake Chany. Our studies have reconstructed the history of these depressions. A model describing their filling with sediments is proposed. The lacustrine sediments penetrated by boreholes and pits are dated by the radiocarbon method at 6.3-2.0 cal. kyr BP. The data obtained explane the long existence of Lake Chany as a shallow basin and rise in its level at ~ 2 kyr BP. © 2018
Ключевые слова: Novosibirsk; Lake Chany; Kargat River; water budget; runoff; radiocarbon dating; paleolimnology; paleohydrology; lake evolution; Holocene; basin analysis; West Siberia; paleolimnology; paleohydrology; lakes; Holocene; basin of Lake Chany; lacustrine deposit; Russian Federation;
Издано: 2018
Физ. характеристика: с.541-555
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