Andradite
| Andradite | |
|---|---|
| 240px
single crystal (4.2cm) - Diakon, Nioro du Sahel Circle, Kayes Region, Mali
|
|
| General | |
| Category | Garnet group |
| Formula (repeating unit) |
Ca3Fe2(SiO4)3 |
| Strunz classification | 09.AD.25 |
| Crystal symmetry | Isometric 4/m 3 2/m |
| Unit cell | a = 12.056 Å; Z = 8 |
| Identification | |
| Color | Yellow, greenish yellow to emerald-green, dark green; brown, brownish red, brownish yellow; grayish black, black; may be sectored |
| Crystal habit | Commonly well-crystallized dodecahedra, trapezohedra, or combinations, also granular to massive |
| Crystal system | Cubic - Hexoctahedral |
| Cleavage | none |
| Fracture | conchoidal to uneven |
| Tenacity | Brittle |
| Mohs scale hardness | 6.5 to 7 |
| Luster | Adamantine to resinous, dull |
| Streak | White |
| Diaphaneity | Transparent to translucent |
| Specific gravity | 3.859 calculated; 3.8 - 3.9 measured |
| Optical properties | Isotropic, typically weakly anisotropic |
| Refractive index | n = 1.887 |
| Absorption spectra | demantoid - 440nm band or complete absorption at 440nm and below, may also have lines at 618, 634, 685, 690nm [1] |
| References | [1][2][3][4] |
| Major varieties | |
| Demantoid | transparent light to dark green to yellow-green |
| Melanite | opaque black |
| Topazolite | transparent to translucent yellow, may show chatoyancy |
Andradite is a species of the garnet group. It is a nesosilicate, with formula Ca3Fe2Si3O12.
Andradite includes three varieties:
- Melanite: Black in color, referred to as "titanian andradite".[5]
- Demantoid: Vivid green in color, one of the most valuable and rare stones in the gemological world.[6]
- Topazolite: Yellow-green in color and sometimes of high enough quality to be cut into a faceted gemstone, it is rarer than demantoid.[6]
It was first described in 1868 for an occurrence in Drammen, Buskerud, Norway.[3][2][6] Andradite was named after the Brazilian statesman, naturalist, professor and poet José Bonifácio de Andrade e Silva (1763–1838).[2][6]
Occurrence
It occurs in skarns developed in contact metamorphosed impure limestones or calcic igneous rocks; in chlorite schists and serpentinites and in alkalic igneous rocks (typically titaniferous). Associated minerals include vesuvianite, chlorite, epidote, spinel, calcite, dolomite and magnetite.[2] It is found in Italy, the Ural Mountains of Russia, Arizona and California and in Dnipropetrovsk Oblast in Ukraine.
As the other garnets andradite crystallizes in the cubic space group [[Ia3d]], with unit-cell parameter of 12.051 Å at 100 K.[7]
The spin structure of andradite contains two mutually canted equivalent antiferromagnetic sublattices [8] below the Néel temperature (TN=11 K [9]).
See also
- garnet
- almandine
- Demantoid
- grossular
- pyrope
- spessartine
- tsavorite
- uvarovite
- geology
- mineral collecting
- mineral
- gemstone
References
- ↑ 1.0 1.1 Gemological Institute of America, GIA Gem Reference Guide 1995, ISBN 0-87311-019-6
- ↑ 2.0 2.1 2.2 2.3 Handbook of Mineralogy
- ↑ 3.0 3.1 Andradite, Mindat.org
- ↑ Webmineral data
- ↑ Melanite, Mindat.org
- ↑ 6.0 6.1 6.2 6.3 Lua error in package.lua at line 80: module 'strict' not found.
- ↑ Thomas Armbruster and Charles A. Geiger (1993): "Andradite crystal chemistry, dynamic X-site disorder and structural strain in silicate garnets." European Journal of Mineralogy v. 5, no. 1, p. 59-71.
- ↑ Danylo Zherebetskyy (2010). Quantum mechanical first principles calculations of the electronic and magnetic structure of Fe-bearing rock-forming silicates, PhD Thesis, Universal Publishers/Dissertation.com, Boca Raton, Florida, USA, p. 136. ISBN 1-59942-316-2.
- ↑ Enver Murad (1984): "Magnetic ordering in andradite." American Mineralogist 69, no. 7-8; pp. 722-24.
