Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes. / Krtvonogov, Sergey; Narantsetseg, Tserendash; Oyunchimeg, Tserentsegmid и др.
в: Chikei/Transactions, Japanese Geomorphological Union, Том 41, № 3, 08.2020, стр. 227-248.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - Geomorphological settings for past increases of the levels of great Mongolian and Mongolia-Russia transboundary lakes
AU - Krtvonogov, Sergey
AU - Narantsetseg, Tserendash
AU - Oyunchimeg, Tserentsegmid
AU - Agatova, Anna
AU - Khazin, Leonid
AU - Nepop, Roman
AU - Zhilich, Snezhana
AU - Kuleshov, Dmitry
AU - Gusev, Victor
N1 - Publisher Copyright: © 2020 Chikei Dojo Saigai Kenkyo Bumon. All rights reserved.
PY - 2020/8
Y1 - 2020/8
N2 - The paper discusses geomorphological aspects of former appearances of huge lakes in the Valley of Great Lakes, the Valley of Gobi Lakes in northwestern and western Mongolia and in depressions of northeastern Mongolia, and partly in bounding Russia. The problem is far from its solution, despite a progress with dating of the lake sediments reflected in recent publications. In the paper, we analyze morphometry of high levels of the lakes visible on the satellite images as series of shorelines, which are very young, not older than the Holocene age. The investigated lakes are terminal basins collecting waters from the catchments of large rivers draining the Altai, Khangai, and Khentey Mountains; two of them form more complicated lake systems: of the Khyargas Lake including several transitional lakes, and of the Torei - Khukh lakes. The discussing reasons for these rises are obviously climatic with possible high influences of the deglaciation processes in the surrounding mountains.
AB - The paper discusses geomorphological aspects of former appearances of huge lakes in the Valley of Great Lakes, the Valley of Gobi Lakes in northwestern and western Mongolia and in depressions of northeastern Mongolia, and partly in bounding Russia. The problem is far from its solution, despite a progress with dating of the lake sediments reflected in recent publications. In the paper, we analyze morphometry of high levels of the lakes visible on the satellite images as series of shorelines, which are very young, not older than the Holocene age. The investigated lakes are terminal basins collecting waters from the catchments of large rivers draining the Altai, Khangai, and Khentey Mountains; two of them form more complicated lake systems: of the Khyargas Lake including several transitional lakes, and of the Torei - Khukh lakes. The discussing reasons for these rises are obviously climatic with possible high influences of the deglaciation processes in the surrounding mountains.
KW - Central Asia
KW - Geomorphology
KW - Lake level changes
KW - Mongolia
KW - Paleolakes
KW - Remote sensing
KW - Russia
KW - Terminal basins
UR - http://www.scopus.com/inward/record.url?scp=85102939089&partnerID=8YFLogxK
M3 - Article
AN - SCOPUS:85102939089
VL - 41
SP - 227
EP - 248
JO - Chikei/Transactions, Japanese Geomorphological Union
JF - Chikei/Transactions, Japanese Geomorphological Union
SN - 0389-1755
IS - 3
ER -
ID: 35675979