The First Find of Mannardite in Russia
- 作者: Reznitsky L.Z.1, Sklyarov E.V.1, Ushchapovskaya Z.F.1, Barash I.G.1
-
隶属关系:
- Institute of the Earth’s Crust, Siberian Branch
- 期: 卷 479, 编号 1 (2018)
- 页面: 397-400
- 栏目: Geochemistry
- URL: https://ogarev-online.ru/1028-334X/article/view/192590
- DOI: https://doi.org/10.1134/S1028334X18030285
- ID: 192590
如何引用文章
详细
Mannardite was found in a type of Cr–V–bearing metamorphic rock of the Slyudyanka complex (South Baikal region). The X-ray data of the mineral are recalculated for three scenarios taking into account possible variations of the mannardite structure. The mean chemical composition is as follows (14 analyses, wt %): 0.11 SiO2, 52.08 TiO2, 6.19 VO2, 13.51 V2O3, 5.50 Cr2O3, 0.24 Al2O3, 0.16 Fe2O3, 0.05 MgO, 20.09 BaO, 2.09 H2O (the H2O, VO2, and V2O3 contents are recalculated). The formula of the mean composition is (Ba1.06H2O0.94)(Ti5.27Si0.21V0.614+V1.453+Cr0.59Fe0.02Mg0.01)O16. Mannardite is characterized by the presence of different valent V. The mineral can be hydrous with molecular H2O or hydroxylion in tunnels or anhydrous. Mannardite can be considered an indicator of the hydroxyl or oxygen regime of petrogenetic processes.
作者简介
L. Reznitsky
Institute of the Earth’s Crust, Siberian Branch
编辑信件的主要联系方式.
Email: reznitskii@mail.ru
俄罗斯联邦, Irkutsk, 664033
E. Sklyarov
Institute of the Earth’s Crust, Siberian Branch
Email: reznitskii@mail.ru
俄罗斯联邦, Irkutsk, 664033
Z. Ushchapovskaya
Institute of the Earth’s Crust, Siberian Branch
Email: reznitskii@mail.ru
俄罗斯联邦, Irkutsk, 664033
I. Barash
Institute of the Earth’s Crust, Siberian Branch
Email: reznitskii@mail.ru
俄罗斯联邦, Irkutsk, 664033
补充文件
