The first dating results for gabbro of the dunite–clinopyroxenite–gabbro complex of the Chistop massif (North Urals)


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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.

作者简介

G. Petrova

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

编辑信件的主要联系方式.
Email: Georg_Petrov@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

Yu. Ronkin

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: Georg_Petrov@mail.ru
俄罗斯联邦, Yekaterinburg, 620016

P. Lvov

Isotope Research Center

Email: Georg_Petrov@mail.ru
俄罗斯联邦, St. Petersburg, 119106

A. Maslov

Zavaritsky Institute of Geology and Geochemistry, Ural Branch

Email: Georg_Petrov@mail.ru
俄罗斯联邦, Yekaterinburg, 620016


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