New data concerning the age and specific features of magmatism of timanides in the southern part of the Lyapin structure (Northern Urals)
- Authors: Petrov G.A.1, Ronkin Y.L.1, Gerdes A.2, Maslov A.V.1
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Affiliations:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Goethe–Universitat, Institut für Geowissenschaften
- Issue: Vol 476, No 2 (2017)
- Pages: 1125-1129
- Section: Geology
- URL: https://journals.rcsi.science/1028-334X/article/view/190983
- DOI: https://doi.org/10.1134/S1028334X17100075
- ID: 190983
Cite item
Abstract
New data on composition and age of Precambrian granites and volcanic rocks in the southern part of the Lyapin structure (Northern Urals) are considered. The geochemical features of the igneous rocks are similar to those of the rocks formed in both divergent and convergent environments. In the Late Precambrian (583–553 Ma), the investigated area is assumed to have been a part of the active margin above the mantle plume.
About the authors
G. A. Petrov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Author for correspondence.
Email: Georg_Petrov@mail.ru
Russian Federation, Yekaterinburg, 620016
Yu. L. Ronkin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: Georg_Petrov@mail.ru
Russian Federation, Yekaterinburg, 620016
A. Gerdes
Goethe–Universitat, Institut für Geowissenschaften
Email: Georg_Petrov@mail.ru
Germany, Frankfurt am Main
A. V. Maslov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: Georg_Petrov@mail.ru
Russian Federation, Yekaterinburg, 620016
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