U–Pb age and geochemistry of zircon inclusions in sapphire: Alkali basaltic source of gems in placers of Primorye
- 作者: Akinin V.V.1, Vysotskiy S.V.2,3, Coble M.4, Aseeva A.V.3
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隶属关系:
- Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
- Far East Federal University
- Far East Geological Institute, Far East Branch
- Stanford University
- 期: 卷 476, 编号 2 (2017)
- 页面: 1173-1176
- 栏目: Geochemistry
- URL: https://journals.rcsi.science/1028-334X/article/view/191065
- DOI: https://doi.org/10.1134/S1028334X17100129
- ID: 191065
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详细
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.
作者简介
V. Akinin
Shilo North-East Interdisciplinary Scientific Research Institute, Far East Branch
Email: vysotskiy@fegi.ru
俄罗斯联邦, Magadan, 685000
S. Vysotskiy
Far East Federal University; Far East Geological Institute, Far East Branch
编辑信件的主要联系方式.
Email: vysotskiy@fegi.ru
俄罗斯联邦, Vladivostok, 690950; Vladivostok, 690022
M. Coble
Stanford University
Email: vysotskiy@fegi.ru
美国, Stanford, CA, 94305
A. Aseeva
Far East Geological Institute, Far East Branch
Email: vysotskiy@fegi.ru
俄罗斯联邦, Vladivostok, 690022
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