Hibonite: Difference between revisions
m →top: dash |
Added short description Tags: Mobile edit Mobile app edit Android app edit App description add |
||
Line 1: | Line 1: | ||
{{Short description|Mineral}} |
|||
{{Infobox mineral |
{{Infobox mineral |
||
| name = Hibonite |
| name = Hibonite |
Latest revision as of 11:53, 27 July 2024
Hibonite | |
---|---|
General | |
Category | Oxide minerals |
Formula (repeating unit) | (Ca,Ce)(Al,Ti,Mg)12O19 |
IMA symbol | Hbn[1] |
Strunz classification | 4.CC.45 |
Crystal system | Hexagonal |
Crystal class |
|
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 | 7+1⁄2–8 |
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 | [2][3] |
Hibonite is a mineral with the chemical formula (Ca,Ce)(Al,Ti,Mg)12O19, occurring in various colours, 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 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.[4] Hibonites were among the first minerals to form as the disk of gas and dust swirling around the young sun cooled.[5]
A very rare gem, hibonite was discovered in 1953 in Madagascar by Paul Hibon, a French prospector.[6]
Colour
[edit]Hibonite can vary in colour, from a bright blue, to green, to orange, to a nearly black deep brown. The colour is related to the degree of oxidation; meteoritic hibonite tends to be blue.[7]
See also
[edit]References
[edit]- ^ Warr, L.N. (2021). "IMA–CNMNC approved mineral symbols". Mineralogical Magazine. 85 (3): 291–320. Bibcode:2021MinM...85..291W. doi:10.1180/mgm.2021.43. S2CID 235729616.
- ^ "Handbook of Mineralogy" (PDF).
- ^ "Hibonite: Hibonite mineral information and data". www.mindat.org.
- ^ "IMA Mineral List with Database of Mineral Properties". rruff.info.
- ^ "A Year in Review and a Look to the Future". Field Museum of Natural History. January 11, 2019. Retrieved 4 December 2021.
- ^ "Hibonite gemstone information". www.gemdat.org.
- ^ Ihinger, Phillip D.; Stolper, Edward (May 1986). "The color of meteoritic hibonite: an indicator of oxygen fugacity". Earth and Planetary Science Letters. 78 (1): 67–79. Bibcode:1986E&PSL..78...67I. doi:10.1016/0012-821X(86)90173-1.