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'''Petalite''', also known as '''castorite''', is a ] ] ] ] ]]]<sub>4</sub>]<sub>10</sub>, crystallizing in the ] system. Petalite is a member of the ] group. It occurs as colorless, grey, yellow, yellow grey, to white tabular crystals and columnar masses. Occurs in lithium-bearing ]s with ], ], and ]. Petalite is an important ore of lithium, and is converted to spodumene and quartz by heating to ~500&nbsp;°C and under 3&nbsp;kbar of pressure in the presence of a dense hydrous alkali borosilicate fluid with a minor carbonate component.<ref>{{cite book|first=W. A. Deer|title=Framework silicates: silica minerals, feldspathoids and the zeolites|year=2004|publisher=Geological Soc.|location=London|isbn=1862391440|pages=296|edition=2. ed.}}</ref> The colorless varieties are often used as ]s. '''Petalite''', also known as '''castorite''', is a ] ] ] ] ]]]<sub>4</sub>]<sub>10</sub>, crystallizing in the ] system. Petalite is a member of the ] group. It occurs as colourless, grey, yellow, yellow grey, to white tabular crystals and columnar masses. Occurs in lithium-bearing ]s with ], ], and ]. Petalite is an important ore of lithium, and is converted to spodumene and quartz by heating to ~500&nbsp;°C and under 3&nbsp;kbar of pressure in the presence of a dense hydrous alkali borosilicate fluid with a minor carbonate component.<ref>{{cite book|first=W. A. Deer|title=Framework silicates: silica minerals, feldspathoids and the zeolites|year=2004|publisher=Geological Soc.|location=London|isbn=1862391440|pages=296|edition=2. ed.}}</ref> The colorless varieties are often used as ]s.
] ]
Discovered in 1800, type locality: ], ], ]. The name is derived from ] petalon for ''leaf''.<ref name=Mindat/> Discovered in 1800, type locality: ], ], ]. The name is derived from ] petalon for ''leaf''.<ref name=Mindat/>

Revision as of 04:30, 24 January 2012

Petalite
Petalite from Minas Gerais State, Brazil (size: 3x4 cm)
General
CategoryTectosilicate
Formula
(repeating unit)
LiAlSi4O10
Strunz classification09.EF.05
Crystal systemMonoclinic
Space groupMonoclinic prismatic
H-M symbol: (2/m)
Space group: P 2/a
Unit cella = 11.737 Å, b = 5.171 Å, c = 7.63 Å; β = 112.54°; Z = 2
Identification
ColorColorless, grey, yellow, pink, to white
Crystal habitTabular prismatic crystals and columnar masses
TwinningCommon on {001}, lamellar
CleavagePerfect on {001}, poor on {201} with 38.5° angle between the two
FractureSubconchoidal
TenacityBrittle
Mohs scale hardness6 - 6.5
LusterVitreous, pearly on cleavages
StreakColorless
DiaphaneityTransparent to translucent
Specific gravity2.4
Optical propertiesBiaxial (+)
Refractive indexnα=1.504, nβ=1.510, nγ=1.516
Birefringenceδ = 0.012
2V angle82 – 84° measured
Melting point1350 °C
Fusibility5
SolubilityInsoluble
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 colourless, 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.

Petalite from Paprok, Nuristan Province, Afghanistan (size: 7.3 x 2.9 x 2.4 cm)

Discovered in 1800, type locality: Utö Island, Haninge, Stockholm, Sweden. The name is derived from Greek petalon for leaf.

References

  1. "Petalite". Digital Fire. Retrieved 23 October 2011.
  2. Handbook of Mineralogy
  3. Webmineral
  4. ^ Mindat
  5. *Hurlbut, Cornelius S. and Klein, Cornelis, 1985, Manual of Mineralogy, Wiley, 20th ed., pp. 459-460 ISBN 0-471-80580-7
  6. Framework silicates: silica minerals, feldspathoids and the zeolites (2. ed. ed.). London: Geological Soc. 2004. p. 296. ISBN 1862391440. {{cite book}}: |edition= has extra text (help); |first= missing |last= (help)


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