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Keywords = Keivy alkaline province

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12 pages, 5384 KiB  
Article
Compositional and Textural Variations in Hainite-(Y) and Batievaite-(Y), Two Rinkite-Group Minerals from the Sakharjok Massif, Keivy Alkaline Province, NW Russia
by Ekaterina A. Selivanova, Lyudmila M. Lyalina and Yevgeny E. Savchenko
Minerals 2018, 8(10), 458; https://doi.org/10.3390/min8100458 - 16 Oct 2018
Cited by 5 | Viewed by 3147
Abstract
Compositional and textural variations in the rinkite group, seidozerite supergroup minerals, batievaite-(Y), hainite-(Y) and close to them titanosilicates from the Sakharjok massif were studied. Statistical analysis allowed for defining two major substitution schemes leading to batievaite-(Y) and cation-deficient titanosilicates forming: Ca2+ + [...] Read more.
Compositional and textural variations in the rinkite group, seidozerite supergroup minerals, batievaite-(Y), hainite-(Y) and close to them titanosilicates from the Sakharjok massif were studied. Statistical analysis allowed for defining two major substitution schemes leading to batievaite-(Y) and cation-deficient titanosilicates forming: Ca2+ + Na+ + F ↔ □ + Y3+ + (OH) and Ca2+ + Na+ ↔ □ + REE3+. Batievaite-(Y) and other cation-deficient titanosilicates are the earlier minerals formed by solid state transformation of the primary full-cation phase. Hainite-(Y) is a later mineral. It forms rims around earlier titanosilicates, or, less often, separate crystals. Full article
(This article belongs to the Special Issue Arctic Mineral Resources: Science and Technology)
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