Email this article The First Quantitative Evaluation Data on Vendian Metamorphism in the Eastern Part of the Bashkir Meganticlinorium
- Authors: Kovalev S.G.1, Puchkov V.N.1, Kovalev S.S.1, Vysotskii S.I.1
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Affiliations:
- Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences
- Issue: Vol 483, No 1 (2018)
- Pages: 1418-1422
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/194312
- DOI: https://doi.org/10.1134/S1028334X1811020X
- ID: 194312
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Abstract
This paper reports the data on the P–T parameters of the Vendian metamorphism within the eastern wing of the Bashkir Meganticlinorium. Regular near-EW variations in the P–T parameters are due to the fact that the Late Vendian Southern Urals developed under compression resulting from orogenic movements in the Timanides fold region. The stress metamorphism is specified by the “near-fault” nature, when the metamorphosed rock zones alternate with unaltered deposits.
About the authors
S. G. Kovalev
Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences
Author for correspondence.
Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077
V. N. Puchkov
Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences
Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077
S. S. Kovalev
Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences
Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077
S. I. Vysotskii
Institute of Geology, Ufa Scientific Center, Russian Academy of Sciences
Email: kovalev@ufaras.ru
Russian Federation, Ufa, 450077
