New evidence of the nonglaciated development of the northern part of the Western Siberian lowland in the Quaternary period
- 作者: Sheinkman V.S.1,2,3, Melnikov V.P.1,2,3, Sedov S.N.1,2,3, Parnachev V.P.2,4
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隶属关系:
- Tyumen State University
- Tyumen Industrial University
- Institute of the Earth’s Cryosphere, Siberian Branch
- National Research Tomsk State University
- 期: 卷 477, 编号 2 (2017)
- 页面: 1430-1433
- 栏目: Geography
- URL: https://ogarev-online.ru/1028-334X/article/view/191632
- DOI: https://doi.org/10.1134/S1028334X17120078
- ID: 191632
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详细
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.
作者简介
V. Sheinkman
Tyumen State University; Tyumen Industrial University; Institute of the Earth’s Cryosphere, Siberian Branch
编辑信件的主要联系方式.
Email: vlad.sheinkman@mail.ru
俄罗斯联邦, Tyumen, 625026; Tyumen, 625026; Tyumen, 625000
V. Melnikov
Tyumen State University; Tyumen Industrial University; Institute of the Earth’s Cryosphere, Siberian Branch
Email: vlad.sheinkman@mail.ru
俄罗斯联邦, Tyumen, 625026; Tyumen, 625026; Tyumen, 625000
S. Sedov
Tyumen State University; Tyumen Industrial University; Institute of the Earth’s Cryosphere, Siberian Branch
Email: vlad.sheinkman@mail.ru
俄罗斯联邦, Tyumen, 625026; Tyumen, 625026; Tyumen, 625000
V. Parnachev
Tyumen Industrial University; National Research Tomsk State University
Email: vlad.sheinkman@mail.ru
俄罗斯联邦, Tyumen, 625026; Tomsk, 634050
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