Structural paragenesises of the flysch complexes in the central part of the Uralian Foredeep
- Authors: Tevelev A.V.1, Tevelev A.V.1, Prudnikov I.A.1, Khotylev A.O.1, Baraboshkin E.E.1, Popov S.S.1
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Affiliations:
- Department of Geology
- Issue: Vol 71, No 4 (2016)
- Pages: 290-295
- Section: Article
- URL: https://journals.rcsi.science/0145-8752/article/view/174285
- DOI: https://doi.org/10.3103/S0145875216040062
- ID: 174285
Cite item
Abstract
The structural features of the Upper Paleozoic flysch formations in the central part of the Cis-Uralian Foredeep were studied. Three types of structural paragenesises typical of thrust zones were distinguished. Among them are west vergent inclined folds and overfolds that pass into recumbent folds near a fault plane, structured tectonic melange, local thrusts, schistosity zones, and flat slipping planes. The various structural elements extend from northwest to northeast, due to the structural heterogeneity of the allochthon, approximately parallel to the strike of the Karantrav thrust.
Keywords
About the authors
Al. V. Tevelev
Department of Geology
Author for correspondence.
Email: atevelev@rambler.ru
Russian Federation, Moscow
Ark. V. Tevelev
Department of Geology
Email: atevelev@rambler.ru
Russian Federation, Moscow
I. A. Prudnikov
Department of Geology
Email: atevelev@rambler.ru
Russian Federation, Moscow
A. O. Khotylev
Department of Geology
Email: atevelev@rambler.ru
Russian Federation, Moscow
E. E. Baraboshkin
Department of Geology
Email: atevelev@rambler.ru
Russian Federation, Moscow
S. S. Popov
Department of Geology
Email: atevelev@rambler.ru
Russian Federation, Moscow