Arsenic-rich nagyagite (up to 5.5 wt % As) has been discovered in samp
les from the Au-Ag-Te deposit of Sacarimb, western Romania. Optical pr
operties of the mineral show small but distinct differences to nagyagi
te (ss). Chemical analyses indicate a substitution of As for Sb, and c
hemical zonation suggests rapid changes in the chemistry of the minera
lising fluids.