The Taratash indenter and its role in the geological structure of the Urals
- Autores: Tevelev A.V.1, Tevelev A.V.1, Fedorchuk V.A.1, Khotylev A.O.1, Kosheleva I.A.1
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Afiliações:
- Department of Geology
- Edição: Volume 72, Nº 2 (2017)
- Páginas: 95-105
- Seção: Article
- URL: https://journal-vniispk.ru/0145-8752/article/view/174397
- DOI: https://doi.org/10.3103/S0145875217020077
- ID: 174397
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Resumo
This work presents the results of studying zones bounded by the Archean and Early Proterozoic Taratash block, which breaks the meridional structure of the Urals, pinching its structural zones at the latitude of the town of Miass. The mesostructures of rupture zones, microtextures of tectonites, anisotropy of the magnetic susceptibility, and seismic-wave propagation rate in blastomylonites were studied. The kinematic history of the Taratash block consists of two phases: (1) exhumation in the Middle Riphean under conditions of crustal extension; and (2) the formation of an indenter in the Late Paleozoic under conditions of compression.
Sobre autores
Al. Tevelev
Department of Geology
Autor responsável pela correspondência
Email: atevelev@rambler.ru
Rússia, Moscow
Ark. Tevelev
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow
V. Fedorchuk
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow
A. Khotylev
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow
I. Kosheleva
Department of Geology
Email: atevelev@rambler.ru
Rússia, Moscow
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