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| formula = LiAlSi<sub>4</sub>O<sub>10</sub> | | formula = LiAlSi<sub>4</sub>O<sub>10</sub> | ||
| molweight = | | molweight = | ||
| strunz = |
| strunz = 9.EF.05 | ||
⚫ | | system = ] | ||
| symmetry = Monoclinic prismatic<br/>]: (2/m) <br/>]: P 2/a | |||
| class = Prismatic (2/m) <br/><small>(same ])</small> | |||
⚫ | | unit cell = a = 11.737 |
||
| symmetry = ''P2/a'' | |||
⚫ | | unit cell = a = 11.737 Å, <br/>b = 5.171 Å, <br/>c = 7.63 Å; <br/>β = 112.54°; Z = 2 | ||
| color = Colorless, grey, yellow, pink, to white | | color = Colorless, grey, yellow, pink, to white | ||
| habit = Tabular prismatic crystals and columnar masses | | habit = Tabular prismatic crystals and columnar masses | ||
⚫ | | system = ] | ||
| twinning = Common on {001}, lamellar | | twinning = Common on {001}, lamellar | ||
| cleavage = Perfect on {001}, poor on {201} with 38.5° angle between the two | | cleavage = Perfect on {001}, poor on {201} with 38.5° angle between the two |
Revision as of 07:01, 5 December 2016
Petalite | |
---|---|
Petalite from Minas Gerais State, Brazil (size: 3x4 cm) | |
General | |
Category | Tectosilicate |
Formula (repeating unit) | LiAlSi4O10 |
Strunz classification | 9.EF.05 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | P2/a |
Unit cell | a = 11.737 Å, b = 5.171 Å, c = 7.63 Å; β = 112.54°; Z = 2 |
Identification | |
Color | Colorless, grey, yellow, pink, to white |
Crystal habit | Tabular prismatic crystals and columnar masses |
Twinning | Common on {001}, lamellar |
Cleavage | Perfect on {001}, poor on {201} with 38.5° angle between the two |
Fracture | Subconchoidal |
Tenacity | Brittle |
Mohs scale hardness | 6 - 6.5 |
Luster | Vitreous, pearly on cleavages |
Streak | Colorless |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.4 |
Optical properties | Biaxial (+) |
Refractive index | nα=1.504, nβ=1.510, nγ=1.516 |
Birefringence | δ = 0.012 |
2V angle | 82 – 84° measured |
Melting point | 1350 °C |
Fusibility | 5 |
Solubility | Insoluble |
References |
Petalite, also known as castorite, is a lithium aluminium tectosilicate mineral LiAlSi4O10, crystallizing in the monoclinic system. Petalite is a member of the feldspathoid group. It occurs as colorless, grey, yellow, yellow grey, to white tabular crystals and columnar masses. Occurs in lithium-bearing pegmatites with spodumene, lepidolite, and tourmaline. Petalite is an important ore of lithium, and is converted to spodumene and quartz by heating to ~500 °C and under 3 kbar of pressure in the presence of a dense hydrous alkali borosilicate fluid with a minor carbonate component. The colorless varieties are often used as gemstones.
Discovery and occurrence
Discovered in 1800, by Brazilian naturalist Jose Bonifacio de Andrada e Silva. Type locality: Utö Island, Haninge, Stockholm, Sweden. The name is derived from the Greek word petalon, which means leaf.
Economic deposits of petalite are found near Kalgoorlie, Western Australia; Aracuai, Minas Gerais, Brazil; Karibib, Namibia; Manitoba, Canada; and Bikita, Zimbabwe.
The first important economic application for petalite was as a raw material for the glass-ceramic cooking ware CorningWare. It has been used as a raw material for ceramic glazes.
References
- "Petalite". Digital Fire. Retrieved 23 October 2011.
- Handbook of Mineralogy
- Webmineral
- ^ Mindat
- *Hurlbut, Cornelius S. and Klein, Cornelis, 1985, Manual of Mineralogy, Wiley, 20th ed., pp. 459-460 ISBN 0-471-80580-7
- Deer, W. A. (2004). Framework silicates: silica minerals, feldspathoids and the zeolites (2. ed.). London: Geological Soc. p. 296. ISBN 1-86239-144-0.
- D'Andraba (1800). "Des caractères et des propriétés de plusieurs nouveaux minérauxde Suède et de Norwège , avec quelques observations chimiques faites sur ces substances". Journal de chimie et de physique. 51: 239.
- Sowerby, James (1811). Exotic mineralogy: Or, Coloured figures of foreign minerals: As a supplement to British mineralogy.
External links
- Media related to Petalite at Wikimedia Commons
- "Petalite" . Encyclopædia Britannica. Vol. 21 (11th ed.). 1911.