Anorthoclase

The mineral anorthoclase ((Na,K)AlSi3O8) is a crystalline solid solution in the alkali feldspar series, in which the sodium-aluminium silicate member exists in larger proportion. It typically consists of between 10 and 36 percent of KAlSi3O8 and between 64 and 90 percent of NaAlSi3O8.

Anorthoclase
Doubly terminated anorthoclase crystal from Kinki Region, Honshu, Japan. Size: 1.3 cm × 0.9 cm × 0.7 cm (0.5 in × 0.4 in × 0.3 in)
General
CategoryFeldspar
Formula
(repeating unit)
(Na,K)AlSi3O8
IMA symbolAno
Strunz classification9.FA.30
Crystal systemTriclinic
Crystal classPinacoidal (1)
(same H–M symbol)
Space groupC1
Unit cella = 8.28, b = 12.97
c = 7.15 [Å]; α = 91.05°
β = 116.26°, γ = 90.15°; Z = 4
Identification
ColorColorless, also white, pale creamy yellow, red, green
Crystal habitShort prismatic crystals; tabular, rhombic, flattened along [010]
TwinningPolysynthetic twinning produces a grid pattern on [100]
CleavagePerfect on [001], other partings
FractureUneven
TenacityBrittle
Mohs scale hardness6
LusterVitreous to pearly on cleavage planes
StreakWhite
DiaphaneityTransparent
Specific gravity2.57–2.60
Optical propertiesBiaxial (−)
Refractive indexnα = 1.519–1.529
nβ = 1.524–1.534
nγ = 1.527–1.536
Birefringenceδ = 0.008
2V angleMeasured: 34°–60°
References
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