Enviar artigo por via de e-mail The first dating results for gabbro of the dunite–clinopyroxenite–gabbro complex of the Chistop massif (North Urals)
- Autores: Petrova G.A.1, Ronkin Y.L.1, Lvov P.A.2, Maslov A.V.1
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Afiliações:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Isotope Research Center
- Edição: Volume 475, Nº 2 (2017)
- Páginas: 926-929
- Seção: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/190539
- DOI: https://doi.org/10.1134/S1028334X17080177
- ID: 190539
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Resumo
The first data on the Late Riphean age by U–Pb and Sm–Nd analysis (≥922 ± 14 and 686 ± 19 Ma, respectively) were obtained for rocks of the dunite–clinopyroxenite–gabbro complex of the Chistop massif in the Patinum-bearing Belt of the Urals. These data allow one to assume that the formation of the Ural paleoocean probably started immediately after the break-up of Rodinia.
Sobre autores
G. Petrova
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
P. Lvov
Isotope Research Center
Email: Georg_Petrov@mail.ru
Rússia, St. Petersburg, 119106
A. Maslov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: Georg_Petrov@mail.ru
Rússia, Yekaterinburg, 620016
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