U–Pb age and geochemistry of zircon inclusions in sapphire: Alkali basaltic source of gems in placers of Primorye


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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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