Cambrian Magmatism in the Northern Urals: New Data on the Age and Formation Conditions


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Resumo

Cambrian igneous formations in the Northern Urals were identified and described for the first time. It was established that the Timanide orogeny terminated in the Early Cambrian and was followed by continental rifting above a mantle plume in the Late Cambrian.

Sobre autores

G. Petrov

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Autor responsável pela correspondência
Email: georg_petrov@mail.ru
Rússia, Yekaterinburg, 620016

Yu. Ronkin

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: georg_petrov@mail.ru
Rússia, Yekaterinburg, 620016

A. Gerdes

Institut für Geowissenschaften Facheinheit Mineralogie-Petrologie und Geochemie

Email: georg_petrov@mail.ru
Alemanha, Frankfurt am Main

A. Maslov

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: georg_petrov@mail.ru
Rússia, Yekaterinburg, 620016

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