U–Pb age and geochemistry of zircon inclusions in sapphire: Alkali basaltic source of gems in placers of Primorye
- Authors: Akinin V.V.1, Vysotskiy S.V.2,3, Coble M.4, Aseeva A.V.3
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Affiliations:
- Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
- Far East Federal University
- Far East Geological Institute, Far East Branch
- Stanford University
- Issue: Vol 476, No 2 (2017)
- Pages: 1173-1176
- Section: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/191065
- DOI: https://doi.org/10.1134/S1028334X17100129
- ID: 191065
Cite item
Abstract
This paper reports the first results of U–Pb SHRIMP dating of zircon inclusions in sapphire from the Nezametninskii placers in the north of Primorye. The obtained age of paragenesis of these minerals (12.2 ± 0.2 Ma) is almost consistent with the age of erupted alkali basalts in the region, thus evidencing their genetic relation. According to the geochemistry data on trace elements, the dated zircon was crystallized from an alkali basaltic magma or its later trachyte/phonolite derivatives.
About the authors
V. V. Akinin
Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
Email: vysotskiy@fegi.ru
Russian Federation, Magadan, 685000
S. V. Vysotskiy
Far East Federal University; Far East Geological Institute, Far East Branch
Author for correspondence.
Email: vysotskiy@fegi.ru
Russian Federation, Vladivostok, 690950; Vladivostok, 690022
M. Coble
Stanford University
Email: vysotskiy@fegi.ru
United States, Stanford, CA, 94305
A. V. Aseeva
Far East Geological Institute, Far East Branch
Email: vysotskiy@fegi.ru
Russian Federation, Vladivostok, 690022
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