Albites | |
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General | |
Category | plagioclase, feldspar, tectosilicate |
Formula (repeating unit) | NaAlSi 3O 8 or Na 1.0–0.9Ca 0.0–0.1Al 1.0–1.1Si 3.0–2.9O 8 |
IMA symbol | Ab[1] |
Strunz classification | 9.FA.35 |
Crystal system | Triclinic |
Crystal class |
|
Space group | C1 |
Unit cell |
|
Identification | |
Color | White to gray, blueish, greenish, reddish; may be chatoyant |
Crystal habit | Crystals commonly tabular, divergent aggregates, granular, cleavable massive |
Twinning | Common giving polysynthetic striae on {001} or {010} also contact, simple and multiple |
Cleavage | Perfect on {001}, very good on {010}, imperfect on {110} |
Fracture | Uneven to conchoidal |
Tenacity | Brittle |
Mohs scale hardness | 6–6.5 |
Luster | Vitreous, typically pearly on cleavages |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.60–2.65 |
Optical properties | Biaxial (+) |
Refractive index |
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Birefringence | δ = 0.010 |
2V angle | 85–90° (low); 52–54° (high) |
Dispersion | r < v weak |
Melting point | 1,100–1,120 °C (2,010–2,050 °F) |
Other characteristics | Low- and high-temperature structural modifications are recognized |
References | [2][3][4] |
Albite is a plagioclase feldspar mineral. It is the sodium endmember of the plagioclase solid solution series. It represents a plagioclase with less than 10% anorthite content. The pure albite endmember has the formula NaAlSi
3O
8. It is a tectosilicate. Its color is usually pure white, hence its name from Latin, albus.[5] It is a common constituent in felsic rocks.