Fassaite Explained
Fassaite |
System: | Monoclinic |
Class: | Prismatic (2/m) (same H-M symbol) |
Symmetry: | C2/c (no. 15) |
Color: | light-dark green, black |
Habit: | prismatic, short, plane |
Mohs: | 6 |
Streak: | greenish-white |
Gravity: | 2.9-3.3 |
References: | [1] |
Fassaite is a variety of augite with a very low iron content, .[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
- Book: Schumann, Walter . BLV Bestimmungsbuch . Mineralien aus aller Welt . 2 . 1991 . 3-405-14003-X . 223 .
Notes and References
- Dowty . E. . Clark . J.R. . American Mineralogist . 58 . 1973 . 230–242 . Crystal structure refinement and optical properties of a Ti3+ fassaite from the Allende Meteorite . 1973AmMin..58..230D . 30 December 2020.
- http://www.mindat.org/min-11019.html Mindat
- http://geosci.uchicago.edu/~grossman/Comparative_study_mel,_fass.pdf 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