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


如何引用文章

全文:

开放存取 开放存取
受限制的访问 ##reader.subscriptionAccessGranted##
受限制的访问 订阅存取

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

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2017