Pseudowollastonite
Pseudowollastonite is a high-temperature mineral phase of CaSiO3 and is polymorphous with wollastonite. Its formula can alternatively be written as Ca3Si3O9. Other names include ß-Wollastonite, and cyclowollastonite.[3][4]
Pseudowollastonite | |
---|---|
General | |
Category | Cyclosilicate |
IMA symbol | Pwo[1] |
Strunz classification | 9.CA.20 |
Crystal system | Monoclinic |
Crystal class | Prismatic (2/m) (same H-M symbol) |
Space group | C2/c |
Identification | |
Luster | Vitreous |
Diaphaneity | Transparent |
References | [2] |
It occurs in high temperature (pyrometamorphic) environments such as the Hatrurim Formation of the Negev Desert[3] and the graphite mine at Pfaffenrenth near Hauzenberg, Bavaria.[5] It also occurs in slags and cement.
References
- 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.
- Mineralienatlas
- Pseudo wollastonite on Mindat.org
- Glossary of Geology, eds. Julia A. Jackson, James P. Mehl, and Klaus K. E. Neuendorf; American Geosciences Institute, 2011, 5th ed., p. 524 ISBN 978-0922152896
- Fleischer, M., 1973, New mineral names: Cyclowollastonite, American Mineralogist: 58: 560
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