Formed as the result of the Alpine metamorphism under greenschist-facies conditions of pre-Tertiary hydrothermal Cu-Bi mineralization. Related to cuprobismutite.
IMA Status:
Approved IMA 2001 (Dana # Added)
Locality:
Piz Grisch Mountain, Val Ferrera, Graub�nden, Switzerland. Link to MinDat.org Location Data.