Svanbergite
Appearance
Svanbergite | |
---|---|
General | |
Category | Phosphate minerals |
Formula (repeating unit) | SrAl3(PO4)(SO4)(OH)6 |
Strunz classification | 8.BL.05 |
Crystal system | Trigonal |
Crystal class | Hexagonal scalenohedral (3m) H-M symbol: (3 2/m) |
Space group | R3m |
Unit cell | a = 6.970–6.992 Å c = 16.567–16.75 Å, Z = 3 |
Identification | |
Color | Colorless, cream-yellow, rose, reddish brown |
Crystal habit | Rhombohedral crystals (to pseudocubic); granular, massive |
Cleavage | Distinct on {0001} |
Mohs scale hardness | 5 |
Luster | Vitreous to adamantine |
Diaphaneity | Translucent |
Specific gravity | 3.22 |
Optical properties | Uniaxial (+) |
Refractive index | nω = 1.631–1.635 nε= 1.646–1.649 |
Birefringence | δ=0.0140-0.0150 |
References | [1][2] |
Svanbergite is a colorless, yellow or reddish mineral with the chemical formula SrAl3(PO4)(SO4)(OH)6. It has rhombohedral crystals.[3]
It was first described for an occurrence in Varmland, Sweden in 1854 and named for Swedish chemist Lars Fredrik Svanberg (1805–1878).[1][2]
It occurs in high aluminium medium-grade metamorphic rocks; in bauxite deposits and from sulfate enriched argillic alteration ( high silica and clay) associated with hydrothermal systems often replacing apatite. It occurs with pyrophyllite, kyanite, andalusite, lazulite, augelite, alunite, kaolinite and quartz.[1]
References
Wikimedia Commons has media related to Svanbergite.
- ^ a b c Mineral Handbook
- ^ a b Webmineral
- ^ Richard V. Gaines, H. Catherine W. Skinner, Eugene E. Foord, Brian Mason, and Abraham Rosenzweig: "Dana's new mineralogy", p. 962. John Wiley & Sons, 1997