The Taratash indenter and its role in the geological structure of the Urals


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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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