In order to evaluate the effects of Te-for-S substitution in the minerals of the argyrodite group, the crystal structure and chemical composition of a crystal of Te-rich canfieldite from the Lengenbach quarry, Binntal, Switzerland, was investigated. The unit-cell parameters are a 11.0003(6) Å and V 1331.1(1) Å 3 . The structure was solved and refined in the space group F43m to R 1 = 0.0308 for 194 independent reflections and 21 parameters. Quantitative analysis led to the chemical formula Ag 8.05 (Sn 1.03 Ge 0.01 ) Σ1.04 (S 3.95 Te 1.95 Se 0.01 ) Σ5.91 , ideally Ag 8 Sn(S,Te) 6 . The crystal structure of Te-rich canfieldite was found to be topologically identical to that of putzite, (Cu 4.7 Ag 3.3 )GeS 6 . Neglecting the short Ag-Ag contacts (due to disorder), the two Ag atoms in the structure can be considered as three-fold (Ag1) and four-fold (Ag2) coordinated. Tin adopts a regular tetrahedral coordination. The refinement of the site-occupancy factor indicates Te to be disordered over the three anion positions (i.e., X1, X2, and X3), with a preference for the X1 site.