Hibonite
Hibonite | |
---|---|
Hibonite, 1.6 cm sharp and lustrous crystal from Esiva eluvials, Maromby Commune, Amboasary District, Anosy (Fort Dauphin) Region, Tuléar (Toliara) Province, Madagascar | |
General | |
Category | Oxide minerals |
Formula (repeating unit) | (Ca,Ce)(Al,Ti,Mg)12O19 |
Strunz classification | 4.CC.45 |
Crystal system | Hexagonal |
Crystal class |
Dihexagonal dipyramidal (6/mmm) H-M symbol: (6/m 2/m 2/m) |
Space group | P63/mmc |
Unit cell | a = 5.56, c = 21.89 [Å]; Z = 2 |
Identification | |
Color | Brownish black to black; reddish brown in thin fragments; blue in meteorite occurrence |
Crystal habit | Prismatic platy to steep pyramidal crystals |
Cleavage | {0001} good, {1010} parting |
Fracture | Subconchoidal |
Mohs scale hardness | 7½-8 |
Luster | Vitreous |
Streak | reddish brown |
Diaphaneity | Semitransparent |
Specific gravity | 3.84 |
Optical properties | Uniaxial (-) |
Refractive index | nω = 1.807(2), nε = 1.79(1) |
Pleochroism | O = brownish gray; E = gray |
References | [1][2] |
Hibonite ((Ca,Ce)(Al,Ti,Mg)12O19) is a brownish black mineral with a hardness of 7.5-8.0 and a hexagonal crystal structure. It is rare, but is found in high-grade metamorphic rocks on Madagascar. Some presolar grains in primitive meteorites consist of hibonite. Hibonite also is a common mineral in the Ca-Al-rich inclusions (CAIs) found in some chondritic meteorites. Hibonite is closely related to hibonite-Fe (IMA 2009-027, ((Fe,Mg)Al12O19)) an alteration mineral from the Allende meteorite.[3]
A very rare gem, Hibonite was discovered in Madagascar by Paul Hibon, a French prospector.[4]
See also
References
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