Chemical U–Th–total Pb dating and structural disorder of monazite-(Ce) from granitoids of the Aduiskii massif, Middle Urals
- Authors: Zamyatin D.A.1,2, Votyakov S.L.1, Fershtater G.B.1, Vishniakova M.D.1
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Affiliations:
- Zavaritsky Institute of Geology and Geochemistry, Ural Branch
- Yeltsin Ural Federal University
- Issue: Vol 476, No 1 (2017)
- Pages: 1033-1037
- Section: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/190785
- DOI: https://doi.org/10.1134/S1028334X17090094
- ID: 190785
Cite item
Abstract
Using the methods of electron probe microanalysis and Raman spectroscopy, the zoning, chemical composition, and disorder in the matrix of accessory monazite extracted from a synplutonic quartz dioritic dyke intruding migmatite, diorite, and fine-granular granite of the Aduiskii massif were studied. It was established that monazite grains contained inner and outer zones. The contributions of chemical and radiation factors to mineral disorder were estimated. The results of chemical U-Th-total Pb dating of mineral are reported. The age 252 ± 4 Ma corresponds to the second maximum of granite formation.
About the authors
D. A. Zamyatin
Zavaritsky Institute of Geology and Geochemistry, Ural Branch; Yeltsin Ural Federal University
Author for correspondence.
Email: zamyatin@igg.uran.ru
Russian Federation, Yekaterinburg; Yekaterinburg
S. L. Votyakov
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: zamyatin@igg.uran.ru
Russian Federation, Yekaterinburg
G. B. Fershtater
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: zamyatin@igg.uran.ru
Russian Federation, Yekaterinburg
M. D. Vishniakova
Zavaritsky Institute of Geology and Geochemistry, Ural Branch
Email: zamyatin@igg.uran.ru
Russian Federation, Yekaterinburg
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