Sanidine
Sanidine is the high temperature form of potassium feldspar with a general formula K(AlSi3O8).[1] Sanidine is found most typically in felsic volcanic rocks such as obsidian, rhyolite and trachyte. Sanidine crystallizes in the monoclinic crystal system. Orthoclase is a monoclinic polymorph stable at lower temperatures. At yet lower temperatures, microcline, a triclinic polymorph of potassium feldspar, is stable.
Sanidine | |
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Sanidine - Puy de Sancy, Monts-Dore massif, Puy-de-Dôme, Auvergne, France. (5x4.5cm) | |
General | |
Category | Feldspar |
Formula (repeating unit) | K(AlSi3O8) |
Strunz classification | 9.FA.30 |
Dana classification | 76.01.01.02 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/m |
Identification | |
Color | Colorless to white |
Crystal habit | Tabular crystals, may be acicular |
Twinning | Carlsbad twinning common |
Cleavage | {001} perfect, {010} good |
Fracture | Uneven |
Tenacity | Brittle |
Mohs scale hardness | 6 |
Luster | Vitreous, pearly on cleavage |
Streak | White |
Diaphaneity | Transparent to translucent |
Specific gravity | 2.52 |
Optical properties | Biaxial (-) |
Refractive index | nα = 1.518 - 1.525 nβ = 1.523 - 1.530 nγ = 1.525 - 1.531 |
Birefringence | δ = 0.007 |
2V angle | Measured: 18° - 42° (low); 15° - 63° (high) |
References | [1][2][3] |
Due to the high temperature and rapid quenching, sanidine can contain more sodium in its structure than the two polymorphs that equilibrated at lower temperatures. Sanidine and high albite constitute a solid solution series with intermediate compositions termed anorthoclase. Exsolution of an albite phase does occur; resulting cryptoperthite can best be observed in electron microprobe images.
References
- "The New IMA List of Minerals – A Work in Progress – Updated: March 2014" (PDF). Archived from the original (PDF) on March 25, 2014.
- http://www.mindat.org/min-3521.html Mindat.org
- http://www.webmineral.com/data/Sanidine.shtml Webmineral data
- Hurlbut, Cornelius S.; Klein, Cornelis, 1985, Manual of Mineralogy, 20th ed., Wiley, ISBN 0-471-80580-7