Fassaite

Ca(Mg,Fe,Al)(Si,Al)2O6Crystal systemMonoclinicCrystal classPrismatic (2/m)
(same H-M symbol)Space groupC2/c (no. 15)IdentificationColorlight-dark green, blackCrystal habitprismatic, short, planeMohs scale hardness6Streakgreenish-whiteSpecific gravity2.9-3.3References[1]

Fassaite is a variety of augite with a very low iron content, Ca(Mg,Fe,Al)(Si,Al)2O6.[2] It is named after the Fassa Valley, Italy.

It is thought to be a contact mineral formed at high temperature on the interface between volcanic rocks and limestone. It is also reported in meteorites.[3]

References

  1. ^ Dowty, E.; Clark, J.R. (1973). "Crystal structure refinement and optical properties of a Ti3+ fassaite from the Allende Meteorite". American Mineralogist. 58: 230–242. Bibcode:1973AmMin..58..230D. Retrieved 30 December 2020.
  2. ^ Mindat
  3. ^ Simon, S. B. and L. Grossman, A comparative study of melilite and fassaite in Types B1 and B2 refractory inclusions, Geochimica et Cosmochimica Acta 70 (2006) 780–798
  • Schumann, Walter (1991). Mineralien aus aller Welt. BLV Bestimmungsbuch (2 ed.). p. 223. ISBN 3-405-14003-X.


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