A Kinematic Model of the Formation of the Sim Trough of the Uralian Foredeep
- Autores: Tevelev A.1, Prudnikov I.1, Tevelev A.1, Khotylev A.1, Volodina E.1
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Afiliações:
- Department of Geology
- Edição: Volume 73, Nº 3 (2018)
- Páginas: 238-246
- Seção: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174704
- DOI: https://doi.org/10.3103/S0145875218030110
- ID: 174704
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Resumo
The structural features and mechanism of the formation of the Sim trough within the Uralian Foredeep, as well as the development of the entire Karatau–Suleiman block, are considered. This wedge-shaped block was subject to lateral extrusion to the north along conjugated strike-slip fault zones under a general latitudinal compression. This factor determined the local meridional compression and latitudinal extension of the block. In the central part of the block, the latitudinal extension was compensated by gradual subsidence, which resulted in the formation of the Sim trough.
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Sobre autores
Al. Tevelev
Department of Geology
Autor responsável pela correspondência
Email: atevelev@rambler.ru
Rússia, Moscow, 119991
I. Prudnikov
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow, 119991
Ark. Tevelev
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow, 119991
A. Khotylev
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow, 119991
E. Volodina
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow, 119991