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Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin. / Krivonogov, S. K.; Gusev, V. A.; Parkhomchuk, E. V. и др.

в: Russian Geology and Geophysics, Том 59, № 5, 01.05.2018, стр. 541-555.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Krivonogov, SK, Gusev, VA, Parkhomchuk, EV & Zhilich, SV 2018, 'Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin', Russian Geology and Geophysics, Том. 59, № 5, стр. 541-555. https://doi.org/10.1016/j.rgg.2018.04.007

APA

Krivonogov, S. K., Gusev, V. A., Parkhomchuk, E. V., & Zhilich, S. V. (2018). Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin. Russian Geology and Geophysics, 59(5), 541-555. https://doi.org/10.1016/j.rgg.2018.04.007

Vancouver

Krivonogov SK, Gusev VA, Parkhomchuk EV, Zhilich SV. 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 май 1;59(5):541-555. doi: 10.1016/j.rgg.2018.04.007

Author

Krivonogov, S. K. ; Gusev, V. A. ; Parkhomchuk, E. V. и др. / Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin. в: Russian Geology and Geophysics. 2018 ; Том 59, № 5. стр. 541-555.

BibTeX

@article{568815a829a34b0382ce64bf1dd430f8,
title = "Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin",
abstract = "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.",
keywords = "basin of Lake Chany, Holocene, lakes, paleohydrology, paleolimnology, West Siberia, SEDIMENTS, HOLOCENE, ARAL SEA",
author = "Krivonogov, {S. K.} and Gusev, {V. A.} and Parkhomchuk, {E. V.} and Zhilich, {S. V.}",
year = "2018",
month = may,
day = "1",
doi = "10.1016/j.rgg.2018.04.007",
language = "English",
volume = "59",
pages = "541--555",
journal = "Russian Geology and Geophysics",
issn = "1068-7971",
publisher = "Elsevier Science B.V.",
number = "5",

}

RIS

TY - JOUR

T1 - Intermediate lakes of the Chulym and Kargat river valleys and their role in the evolution of the Lake Chany basin

AU - Krivonogov, S. K.

AU - Gusev, V. A.

AU - Parkhomchuk, E. V.

AU - Zhilich, S. V.

PY - 2018/5/1

Y1 - 2018/5/1

N2 - 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.

AB - 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.

KW - basin of Lake Chany

KW - Holocene

KW - lakes

KW - paleohydrology

KW - paleolimnology

KW - West Siberia

KW - SEDIMENTS

KW - HOLOCENE

KW - ARAL SEA

UR - http://www.scopus.com/inward/record.url?scp=85046633606&partnerID=8YFLogxK

U2 - 10.1016/j.rgg.2018.04.007

DO - 10.1016/j.rgg.2018.04.007

M3 - Article

AN - SCOPUS:85046633606

VL - 59

SP - 541

EP - 555

JO - Russian Geology and Geophysics

JF - Russian Geology and Geophysics

SN - 1068-7971

IS - 5

ER -

ID: 13331693