Tellurantimony, Sb2Te3 has been recorded for the first time in Europe.
It occurs in the epithermal precious metal deposits of western Romani
a: Nagyag (now Sacaramb), Stanija, and Magura-Hondd. The optical prope
rties, chemical composition, and mineral associations of the tellurant
imony are described. Significant contents of Pb, Au, Ag, and As have b
een noted, and these seem to be related to the specific occurrence and
association. The tellurantimony-bearing assemblages probably formed u
nder conditions of high f(Te2) and mean to low f(S2).