The first dating results for gabbro of the dunite–clinopyroxenite–gabbro complex of the Chistop massif (North Urals)
- 作者: Petrova G.1, Ronkin Y.1, Lvov P.2, Maslov A.1
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隶属关系:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Isotope Research Center
- 期: 卷 475, 编号 2 (2017)
- 页面: 926-929
- 栏目: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/190539
- DOI: https://doi.org/10.1134/S1028334X17080177
- ID: 190539
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详细
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