Albite
| Albite | |
|---|---|
_Island,_Greece.jpg) Albite from Crete, scale = 1 in. | |
| General | |
| Category | plagioclase, feldspar, tectosilicate |
| Formula (repeating unit) | NaAlSi3O8 or Na1.0–0.9Ca0.0–0.1Al1.0–1.1Si3.0–2.9O8 |
| Strunz classification | 9.FA.35 |
| Crystal system | Triclinic |
| Crystal class | Pinacoidal (1) (same H-M symbol) |
| Space group | C1 |
| Unit cell | a = 8.16, b = 12.87 c = 7.11 [Å]; α = 93.45° β = 116.4°, γ = 90.28°; Z = 4 |
| 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 | nα = 1.528–1.533 nβ = 1.532–1.537 nγ = 1.538–1.542 |
| Birefringence | δ = 0.010 |
| 2V angle | 85–90° (low); 52–54° (high) |
| Dispersion | r < v weak |
| Melting point | 1100-1120 °C |
| Other characteristics | Low- and high-temperature structural modifications are recognized |
| References | [1][2][3] |
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 NaAlSi3O8. It is a tectosilicate. Its color is usually pure white, hence its name from Latin albus.[4] It is a common constituent in felsic rocks.
Properties
Albite crystallizes with triclinic pinacoidal forms. Its specific gravity is about 2.62 and it has a Mohs hardness of 6–6.5. Albite almost always exhibits crystal twinning often as minute parallel striations on the crystal face. Albite often occurs as fine parallel segregations alternating with pink microcline in perthite as a result of exolution on cooling.
There are two variants of albite, which are referred to as low albite and high albite; the latter is also known as analbite. Although both variants are triclinic, they differ in the volume of their unit cell, which is slightly larger for the high form. The high form can be produced from the low form by heating above c. 750 °C (1382 °F).[5] Upon further heating to more than c. 1050 °C the crystal symmetry changes from triclinic to monoclinic; this variant is also known as monalbite.[6] Albite melts at 1100-1120 °C.[7]
Occurrence
It occurs in granitic and pegmatite masses, in some hydrothermal vein deposits and forms part of the typical greenschist metamorphic facies for rocks of originally basaltic composition.
Discovery
It was first reported in 1815 for an occurrence in Finnbo, Falun, Dalarna, Sweden.[2]
Use
Albite is used as a gemstone, albeit semi-precious. Albite is also used by geologists as it is identified as an important rock forming mineral. There is some industrial use for the mineral such as the manufacture of glass and ceramics. [8][9]
References
- ^ http://rruff.geo.arizona.edu/doclib/hom/albite.pdf Handbook of Mineralogy
- ^ a b http://www.mindat.org/min-96.html Mindat.org
- ^ http://www.webmineral.com/data/Albite.shtml Webmineral data
- ^ One or more of the preceding sentences incorporates text from a publication now in the public domain: Chisholm, Hugh, ed. (1911). "Albite". Encyclopædia Britannica (11th ed.). Cambridge University Press.
- ^ O.F. Tuttle, N.L. Bowen (1950): High-temperature albite and contiguous feldspars. J. Geol. 58(5), 572–583, https://www.jstor.org/stable/30068571
- ^ Monalbite on Mindat
- ^ J.P. Greenwood, P.C. Hess (1998): Congruent melting of albite: theory and experiment. J. Geophysical Research. 103(B12), 29815-29828
- ^ Loose Gemstone Guide – Secrets of the Gem Revealed By Pao Nipperkin
- ^ "Uses of albite". britannica.com. Retrieved 4 April 2019.
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