Pseudowollastonite Explained

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.

Notes and References

  1. Warr. L.N.. 2021. IMA–CNMNC approved mineral symbols. Mineralogical Magazine. 85. 3 . 291–320. 10.1180/mgm.2021.43 . 2021MinM...85..291W . 235729616 . free.
  2. https://www.mineralienatlas.de/lexikon/index.php/MineralData?mineral=Pseudowollastonite Mineralienatlas
  3. http://www.mindat.org/min-9535.html Pseudo wollastonite on Mindat.org
  4. Glossary of Geology, eds. Julia A. Jackson, James P. Mehl, and Klaus K. E. Neuendorf; American Geosciences Institute, 2011, 5th ed., p. 524
  5. Fleischer, M., 1973, New mineral names: Cyclowollastonite, American Mineralogist: 58: 560