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Hibonite is a mineral with the chemical formula (Ca,Ce)(Al,Ti,Mg)
12
O
19
, 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)Al
12
O
19
)
) an alteration mineral from the Allende meteorite.[3]

A very rare gem, hibonite was discovered in 1953 in Madagascar by Paul Hibon, a French prospector.[4]

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.[5]

See also[edit]

References[edit]

  1. ^ "Handbook of Mineralogy" (PDF).
  2. ^ "Hibonite: Hibonite mineral information and data". www.mindat.org.
  3. ^ "IMA Mineral List with Database of Mineral Properties". rruff.info.
  4. ^ "Hibonite gemstone information". www.gemdat.org.
  5. ^ 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. doi:10.1016/0012-821X(86)90173-1.