Intermediate Lakes of the Chulym and Kargat River Valleys and Their Role in the Evolution of the Lake Chany Basin | Sciact - CRIS-система Института катализа

Intermediate Lakes of the Chulym and Kargat River Valleys and Their Role in the Evolution of the Lake Chany Basin Научная публикация

Журнал

Russian Geology and Geophysics
ISSN: 1068-7971

Вых. Данные

Год: 2018, Том: 59, Номер: 5, Страницы: 541-555 Страниц : 15 DOI: 10.1016/j.rgg.2018.04.007

Ключевые слова

paleolimnology; paleohydrology; lakes; Holocene; West Siberia; basin of Lake Chany

Авторы

Krivonogov S.K. ^1,2 , Gusev V.A. ^1,2 , Parkhomchuk E.V. ^2,3 , Zhilich S.V. ^1,4

Организации

1	V.S. Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Koptyuga 3, Novosibirsk, 630090, Russia
2	Novosibirsk State University, ul. Pirogova 2, Novosibirsk, 630090, Russia
3	G.K. Boreskov Institute of Catalysis, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrent’eva 5, Novosibirsk, 630090, Russia
4	Institute of Archeology and Ethnography, Siberian Branch of the Russian Academy of Sciences, pr. Akademika Lavrent’eva 17, Novosibirsk, 630090, Russia

Информация о финансировании (4)

1	Российский фонд фундаментальных исследований	15-05-00678 (115013010277)
2	Российский фонд фундаментальных исследований	16-05-00369 (АААА-А16-116020110168-1)
3	Российский фонд фундаментальных исследований	17-45-540527 (АААА-А17-117062710048-9)
4	Министерство образования и науки Российской Федерации	14.Y26.31.0018 (АААА-А17-117051050004-4)

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.

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. V.59. N5. P.541-555. DOI: 10.1016/j.rgg.2018.04.007 WOS Scopus РИНЦ OpenAlex

Кривоногов С.К. , Гусев В.А. , Пархомчук Е.В. , Жилич С.В.
Промежуточные озера долин рек Чулым и Каргат и их роль в эволюции бассейна озера Чаны
Геология и геофизика. 2018. Т.59. №5. С.673-689. DOI: 10.15372/gig20180507RSCI РИНЦ OpenAlex

Поступила в редакцию:	16 февр. 2017 г.
Принята к публикации:	20 сент. 2017 г.
Опубликована в печати:	1 мая 2018 г.
Опубликована online:	3 мая 2018 г.

Web of science:	WOS:000432475000007
Scopus:	2-s2.0-85046633606
РИНЦ:	35520811
OpenAlex:	W2801602227

БД	Цитирований
Web of science	7
Scopus	8
РИНЦ	9
OpenAlex	9