Ba-dominant fluoroaluminates from the Katugin rare-metal deposit (Transbaikalia, Russia)
- 作者: Starikova A.E.1,2, Sharygin V.V.1,2, Sklyarov E.V.3,4
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隶属关系:
- Sobolev Institute of Geology and Mineralogy, Siberian Branch
- Novosibirsk State University
- Institute of the Earth’s Crust, Siberian Branch
- Far East Federal University
- 期: 卷 472, 编号 1 (2017)
- 页面: 67-71
- 栏目: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/189393
- DOI: https://doi.org/10.1134/S1028334X17010184
- ID: 189393
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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
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