Pseudowollastonite | |
Category: | Cyclosilicate |
Imasymbol: | Pwo[1] |
Strunz: | 9.CA.20 |
System: | Monoclinic |
Class: | Prismatic (2/m) (same H-M symbol) |
Symmetry: | C2/c |
Luster: | Vitreous |
Diaphaneity: | Transparent |
References: | [2] |
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]
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.