Pyroxferroite

Pyroxferroite
Pyroxferroite
General
CategoryInosilicate
Formula
(repeating unit)
(Fe2+,Ca)SiO3
IMA symbolPxf[1]
Strunz classification9.DO.05
Crystal systemTriclinic
Space groupP1 (no. 2)
Unit cella = 6.6213 Å,
b = 7.5506 Å,
c = 17.3806 Å,
α = 114.267°, β = 82.684°, γ = 94.756°, Z = 14
Identification
ColorYellow
CleavageGood on (010), poor on (001)
Mohs scale hardness4.5–5.5
LusterVitreous
StreakWhite
Specific gravity3.68–3.76 g/cm3 (measured)
Optical propertiesBiaxial (+)
Refractive indexnα = 1.748–1.756
nβ = 1.750–1.758
nγ = 1.767–1.768
PleochroismFaint; pale yellow to yellow-orange
2V angle34–40°
References[2][3][4][5][6]

Pyroxferroite (Fe2+,Ca)SiO3 is a single chain inosilicate. It is mostly composed of iron, silicon and oxygen, with smaller fractions of calcium and several other metals.[2] Together with armalcolite and tranquillityite, it is one of the three minerals which were discovered on the Moon during the 1969 Apollo 11 mission. It was then found in Lunar and Martian meteorites as well as a mineral in the Earth's crust. Pyroxferroite can also be produced by annealing synthetic clinopyroxene at high pressures and temperatures. The mineral is metastable and gradually decomposes at ambient conditions, but this process can take billions of years.

  1. ^ 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.
  2. ^ a b "Pyroxferroite" (PDF). Handbook of Mineralogy. Retrieved 2009-08-07.
  3. ^ "Pyroxferroite". Mindat.org. Retrieved 2010-08-07.
  4. ^ "Pyroxferroite". Webmineral. Retrieved 2010-08-07.
  5. ^ Chao, E. C. T.; et al. (1970). "Pyrox-ferrite, a new calcium-bearing iron silicate from Tranquillity Base". Geochimica et Cosmochimica Acta Supplement. 1: 65. Bibcode:1970GeCAS...1...65C.
  6. ^ Windley, B.F. (1973). "Proceedings of the Second Lunar Science Conference". Journal of Geology. 81 (4): 523–524. Bibcode:1973JG.....81..523W. doi:10.1086/627901.

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