The First U–Pb Isotopic Systematics of Natural Aeschynite and Coexisting Monazite
- Autores: Ronkin Y.1, Murzin V.1, Gerdes A.2, Maslov A.1, Varlamov D.3
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Afiliações:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Institut für Geowissenschaften, Facheinheit Mineralogie–Petrologie und Geochemie
- Institute of Experimental Mineralogy
- Edição: Volume 478, Nº 1 (2018)
- Páginas: 82-87
- Seção: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/191981
- DOI: https://doi.org/10.1134/S1028334X18010178
- ID: 191981
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Resumo
We have been the first to study in situ the U–Pb isotopic system of aeschynite identified in the gold-bearing magnetite–chlorite–dolomite rocks of the Karabash serpentine massif in the Southern Urals. In the concordia diagram, the U–Pb LA–ICP–MS data on aeschynite are characterized by a considerable discordance, which is consistent with the regression line, the lower crossing of which with the concordia corresponds to an age of 298 ± 18 Ma, whereas the figurative ellipses of coexisting monazite reveal an almost concordant cluster corresponding to the U–Pb age of 317.3 ± 3.3 Ma. It has been established that the closure temperature of the aeschynite system is lower than that of the coexisting monazite.
Sobre autores
Yu. Ronkin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Autor responsável pela correspondência
Email: y-ronkin@mail.ru
Rússia, Yekaterinburg, 620016
V. Murzin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: y-ronkin@mail.ru
Rússia, Yekaterinburg, 620016
A. Gerdes
Institut für Geowissenschaften, Facheinheit Mineralogie–Petrologie und Geochemie
Email: y-ronkin@mail.ru
Alemanha, Frankfurt am Main
A. Maslov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: y-ronkin@mail.ru
Rússia, Yekaterinburg, 620016
D. Varlamov
Institute of Experimental Mineralogy
Email: y-ronkin@mail.ru
Rússia, Chernogolovka, Moscow oblast, 142432