Deep structure of the South Kara sedimentary basin
- 作者: Rodnikov A.1, Zabarinskaya L.1, Piip V.2, Sergeyeva N.1
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隶属关系:
- Geophysical Center
- Department of Geology
- 期: 卷 10, 编号 1 (2016)
- 页面: 28-33
- 栏目: Article
- URL: https://journals.rcsi.science/1819-7140/article/view/211043
- DOI: https://doi.org/10.1134/S1819714016010073
- ID: 211043
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详细
The structure and evolution of the passive continental margins of the Arctic Ocean are considered on the example of the South Kara Basin. Its development is associated with the evolution of the West Siberian Plate and the formation of the Arctic Ocean. Until the Late Cretaceous, the South Kara Basin was the north margin of the West Siberian Plate, whose formation is related to the Permian–Triassic processes of riftogenesis accompanied by the eruptions of traps. In the Mesozoic, due to the opening of the Arctic Ocean, the South Kara basin became a part of the continental margin, where the accumulation of marine sandy–clayey rocks continued.
作者简介
A. Rodnikov
Geophysical Center
Email: n.sergeyeva@gcras.ru
俄罗斯联邦, Moscow
L. Zabarinskaya
Geophysical Center
Email: n.sergeyeva@gcras.ru
俄罗斯联邦, Moscow
V. Piip
Department of Geology
Email: n.sergeyeva@gcras.ru
俄罗斯联邦, Moscow
N. Sergeyeva
Geophysical Center
编辑信件的主要联系方式.
Email: n.sergeyeva@gcras.ru
俄罗斯联邦, Moscow