Ba-dominant fluoroaluminates from the Katugin rare-metal deposit (Transbaikalia, Russia)


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

Multiphase aluminofluoride segregations were registered in aegirine–amphibole granite from the Vostochnyi massif of the Katugin rare-metal deposit. Among them are fluorides (fluorite), Ca–Na–Mg fluoraluminates (weberite, cryolite, pachnolite–thomsenolite, prosopite, gearksutite, ralstonite, and others), and Ba fluoraluminates, which had not been observed previously in this massif. Four fluoraluminates with high concentrations of Ba were found in aluminofluoride segregations: usovite Ba2CaMgAl2F14, the most abundant phase, and three potentially new minerals (BaAlF4(OH), BaCa2AlF9, and BaCa4AlF13). The chemical composition of Ba phases and the results of their Raman spectroscopic study are reported.

作者简介

A. Starikova

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

编辑信件的主要联系方式.
Email: a_sklr@mail.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

V. Sharygin

Sobolev Institute of Geology and Mineralogy, Siberian Branch; Novosibirsk State University

Email: a_sklr@mail.ru
俄罗斯联邦, Novosibirsk, 630090; Novosibirsk

E. Sklyarov

Institute of the Earth’s Crust, Siberian Branch; Far East Federal University

Email: a_sklr@mail.ru
俄罗斯联邦, Irkutsk, 664033; Vladivostok

补充文件

附件文件
动作
1. JATS XML

版权所有 © Pleiades Publishing, Ltd., 2017