U–Pb age and geochemistry of zircon inclusions in sapphire: Alkali basaltic source of gems in placers of Primorye
- Авторы: Akinin V.V.1, Vysotskiy S.V.2,3, Coble M.4, Aseeva A.V.3
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Учреждения:
- Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
- Far East Federal University
- Far East Geological Institute, Far East Branch
- Stanford University
- Выпуск: Том 476, № 2 (2017)
- Страницы: 1173-1176
- Раздел: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/191065
- DOI: https://doi.org/10.1134/S1028334X17100129
- ID: 191065
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Аннотация
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.
Об авторах
V. Akinin
Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
Email: vysotskiy@fegi.ru
Россия, Magadan, 685000
S. Vysotskiy
Far East Federal University; Far East Geological Institute, Far East Branch
Автор, ответственный за переписку.
Email: vysotskiy@fegi.ru
Россия, Vladivostok, 690950; Vladivostok, 690022
M. Coble
Stanford University
Email: vysotskiy@fegi.ru
США, Stanford, CA, 94305
A. Aseeva
Far East Geological Institute, Far East Branch
Email: vysotskiy@fegi.ru
Россия, Vladivostok, 690022
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