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From Wikipedia, the free encyclopedia
Yegorovite, ([Na4[Si4O8(OH)4]·7H2O]) is a silicate mineral found in a hyperalkaline pegmatite in the Lovozero Pluton at Mt. Kedykverpakhk in the Kola Peninsula of Russia. It was named in memory of Russian crystallographer Yurii Kavdievich Yegorov-Tismenko, and approved by the Commission on New Minerals and Mineral Names, International Mineralogical Association in 2008.[1]
Yegorovite | |
---|---|
General | |
Category | Silicate mineral |
Formula (repeating unit) | Na4[Si4O8(OH)4]·7H2O |
IMA symbol | Yeg |
Strunz classification | 09.DX.00 |
Dana classification | 65.01.09.01 |
Crystal system | Monoclinic |
Crystal class | Prismatic H–M symbol: (2/m) |
Space group | P22/c |
Unit cell | a = 9.866(7) Å, b = 12.385(5) Å, c = 14.921(1) Å, β = 104.79(6)°, V = 1762(3)ų |
Identification | |
Color | colorless |
Twinning | Polysynthetic |
Cleavage | perfect on {(010) and (001)} |
Fracture | splintery |
Mohs scale hardness | 2 |
Luster | Vitreous |
Streak | white |
Diaphaneity | Opaque |
Specific gravity | 1.90 |
Density | 1.90(2) g/cm³ |
Optical properties | biaxial (−) |
Birefringence | δ = 0.008 |
References | [1][2] |
Yegorovite is colorless, with a white streak. Found in small quantities among pegmatites. It is a natural silicate of alkali cations.[1][2]
The chemical composition of yegorovite in elemental weight percent is as follows:
element | weight % |
---|---|
Na2O | 23.28 |
SiO2 | 45.45 |
H2O | 31.27 |
Total | 100.0 |
The crystal structure of yegorovite is made up of a single chain of four silicon (Si) tetrahedrons [Si4O8(OH)4]∞ and sixfold polyhedrons of [NaO(OH)2(H2O)3] and [NaO(OH)(H2O)4] centered by sodium (Na).
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