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...

Full description

Bibliographic Details
Published in:Doklady Earth Sciences
Main Authors: Sheinkman, V. S., Sedov, S. N., Parnachev, Valerij Petrovich, Melnikov, V. P.
Format: Article in Journal/Newspaper
Language:English
Published: 2017
Subjects:
Западно-Сибирская низменность
четвертичный период
криогенные явления
Ice Sheet
Siberia
Online Access:https://doi.org/10.1134/S1028334X17120078
http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000646386
id fttomskstateuniv:vtls:000646386
record_format openpolar
spelling fttomskstateuniv:vtls:000646386 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 http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000646386 eng eng 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 fttomskstateuniv https://doi.org/10.1134/S1028334X17120078 2019-05-17T19:54:58Z 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 Tomsk State University Research Library Doklady Earth Sciences 477 2 1430 1433
institution Open Polar
collection Tomsk State University Research Library
op_collection_id fttomskstateuniv
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
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
http://vital.lib.tsu.ru/vital/access/manager/Repository/vtls:000646386
genre Ice Sheet
Siberia
genre_facet Ice Sheet
Siberia
op_source Doklady Earth Sciences. 2017. Vol. 477
part 2. P. 1430-1433
op_doi https://doi.org/10.1134/S1028334X17120078
container_title Doklady Earth Sciences
container_volume 477
container_issue 2
container_start_page 1430
op_container_end_page 1433
_version_ 1766030615796252672

Similar Items