Sillimanite: Difference between revisions
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==See also== |
==See also== |
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*Sterlin Johnson |
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*[[List of minerals]] |
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*Sterlin Johnson II |
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*[[List of minerals named after people]] |
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*Sterlin Johnson III |
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*[[kyanite]] |
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*Sterlin Johnson IV |
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*[[andalusite]] |
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==References== |
==References== |
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Revision as of 19:45, 9 February 2012
| Sillimanite | |
|---|---|
 Sillimanite | |
| General | |
| Category | Silicate mineral |
| Formula (repeating unit) | Al2SiO7 |
| Strunz classification | 09.AF.05 |
| Dana classification | 52.02.02a.01 |
| Crystal system | Orthorhombic - Dipyramidal |
| Space group | Orthorhombic (2/m 2/m 2/m) |
| Unit cell | a = 7.47 Å, b = 7.66 Å, c = 5.75 Å; Z=4 |
| Identification | |
| Color | Colorless or white to gray, also brown, yellow, yellow-green, gray-green, blue-green, blue; colorless in thin section |
| Crystal habit | Prismatic crystals, fibrous, acicular |
| Cleavage | {010} perfect |
| Fracture | Splintery |
| Tenacity | Tough |
| Mohs scale hardness | 7 |
| Luster | Vitreous to subadamantine, silky |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 3.24 |
| Optical properties | Biaxial (+) |
| Refractive index | nα = 1.653 - 1.661 nβ = 1.654 - 1.670 nγ = 1.669 - 1.684 |
| Pleochroism | Colorless to pale brown to yellow |
| 2V angle | 21 - 30° |
| References | [1][2][3] |
Sillimanite is an alumino-silicate mineral with the chemical formula Al2SiO7. Sillimanite is named after the American chemist Benjamin Silliman (1779-1864). It was first described in 1824 for an occurrence in Chester, Middlesex County, Connecticut, USA.[3]
Occurrence
Sillimanite is one of three alumino-silicate polymorphs, the other two being andalusite and kyanite. A common variety of sillimanite is known as fibrolite, so named because the mineral appears like a bunch of fibres twisted together when viewed in thin section or even by the naked eye. Both the fibrous and traditional forms of sillimanite are common in metamorphosed sedimentary rocks. It is an index mineral indicating high-temperature metamorphism. It occurs with andalusite, kyanite, potassium feldspar, almandine, cordierite, biotite and quartz in schist, gneiss, hornfels and also rarely in pegmatites.[2]
Sillimanite has been found in Brandywine Springs, New Castle County, Delaware, USA. It was named by the State Legislature in 1977 as the state mineral of Delaware by suggestion of the Delaware Mineralogical Society, Inc.[4]
Natural sillimanite rocks cut into the required shape and size are used mainly in glass industries. Sillimanite is the best raw material for the manufacture of high alumina refractories or 55-60 % alumina bricks. But its use on large scale is not possible due to its fine grading and high cost.[citation needed] Dumortierite and mullite are similar mineral species used in quality porcelain.[5]
See also
- Sterlin Johnson
- Sterlin Johnson II
- Sterlin Johnson III
- Sterlin Johnson IV
References
- ^ "WebMineral entry". Retrieved 2009-12-19.
- ^ a b http://rruff.geo.arizona.edu/doclib/hom/sillimanite.pdf Handbook of Mineralogy
- ^ a b http://www.mindat.org/min-3662.html Mindat.org
- ^ http://www.dgs.udel.edu/Geology/Mineralogy/destatemineral.aspx Delaware State Mineral, Sillimanite, Delaware Geological Survey
- ^ Klein, Cornelis and Cornelius S. Hurlbut, Jr., Manual of Mineralogy, 1985, Wiley 20th ed., p. 380 ISBN 0-471-80580-7
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