Petalite | |
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![]() Petalite from Minas Gerais State, Brazil (size: 3x4 cm) | |
General | |
Category | Phyllosilicate |
Formula (repeating unit) | LiAlSi4O10 |
IMA symbol | Ptl[1] |
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[2] |
Fusibility | 5 |
Solubility | Insoluble |
References | [3][4][5][6] |
Petalite, also known as castorite, is a lithium aluminum phyllosilicate[7] mineral LiAlSi4O10, crystallizing in the monoclinic system. Petalite occurs as colorless, pink, grey, yellow, yellow grey, to white tabular crystals and columnar masses. It 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.[8] Petalite (and secondary spodumene formed from it) is lower in iron than primary spodumene, making it a more useful source of lithium in, e.g., the production of glass. The colorless varieties are often used as gemstones. [citation needed]