New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period
To solve the controversially debated problem related to the areal extent of the ice sheet in Western Siberia in the Quaternary period, we have studied the development of cold born objects of this area estimating the relationships between them in terms of cryogenic diversity. We have obtained a field...
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ftneicon:oai:rour.neicon.ru:rour/274262 2023-05-15T16:40:14+02:00 New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period Sheinkman, V. S. Sedov, S. N. Parnachev, Valerij Petrovich Melnikov, V. P. 2017 application/pdf https://doi.org/10.1134/S1028334X17120078 https://openrepository.ru/article?id=274262 eng eng vtls:000646386 doi:10.1134/S1028334X17120078 https://openrepository.ru/article?id=274262 Doklady Earth Sciences. 2017. Vol. 477, part 2. P. 1430-1433 Западно-Сибирская низменность четвертичный период криогенные явления статьи в журналах info:eu-repo/semantics/article 2017 ftneicon https://doi.org/10.1134/S1028334X17120078 2020-07-21T12:26:35Z To solve the controversially debated problem related to the areal extent of the ice sheet in Western Siberia in the Quaternary period, we have studied the development of cold born objects of this area estimating the relationships between them in terms of cryogenic diversity. We have obtained a field of new cross data related to the development of cryogenic and glacial phenomena, their relationship, and traces they left. The research showed that, in this area, the trend of rock freezing is clearly reflected in the Quaternary formations, but there were no conditions for ice sheet development even during the cryochrons. Article in Journal/Newspaper Ice Sheet Siberia NORA (National aggregator of open repositories of Russian universities) Doklady Earth Sciences 477 2 1430 1433 |
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Open Polar |
collection |
NORA (National aggregator of open repositories of Russian universities) |
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ftneicon |
language |
English |
topic |
Западно-Сибирская низменность четвертичный период криогенные явления |
spellingShingle |
Западно-Сибирская низменность четвертичный период криогенные явления Sheinkman, V. S. Sedov, S. N. Parnachev, Valerij Petrovich Melnikov, V. P. New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
topic_facet |
Западно-Сибирская низменность четвертичный период криогенные явления |
description |
To solve the controversially debated problem related to the areal extent of the ice sheet in Western Siberia in the Quaternary period, we have studied the development of cold born objects of this area estimating the relationships between them in terms of cryogenic diversity. We have obtained a field of new cross data related to the development of cryogenic and glacial phenomena, their relationship, and traces they left. The research showed that, in this area, the trend of rock freezing is clearly reflected in the Quaternary formations, but there were no conditions for ice sheet development even during the cryochrons. |
format |
Article in Journal/Newspaper |
author |
Sheinkman, V. S. Sedov, S. N. Parnachev, Valerij Petrovich Melnikov, V. P. |
author_facet |
Sheinkman, V. S. Sedov, S. N. Parnachev, Valerij Petrovich Melnikov, V. P. |
author_sort |
Sheinkman, V. S. |
title |
New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
title_short |
New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
title_full |
New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
title_fullStr |
New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
title_full_unstemmed |
New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period |
title_sort |
new evidence of the nonglaciated development of the northern part of the western siberian lowland in the quaternary period |
publishDate |
2017 |
url |
https://doi.org/10.1134/S1028334X17120078 https://openrepository.ru/article?id=274262 |
genre |
Ice Sheet Siberia |
genre_facet |
Ice Sheet Siberia |
op_source |
Doklady Earth Sciences. 2017. Vol. 477, part 2. P. 1430-1433 |
op_relation |
vtls:000646386 doi:10.1134/S1028334X17120078 https://openrepository.ru/article?id=274262 |
op_doi |
https://doi.org/10.1134/S1028334X17120078 |
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Doklady Earth Sciences |
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477 |
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2 |
container_start_page |
1430 |
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1433 |
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1766030615614849024 |