Benjamin N. SchumerRobert T. DownsKenneth J. DomanikMarcelo B. AndradeMarcus J. Origlieri
Pirquitasite, ideally Ag 2 ZnSnS 4 (disilver zinc tin tetrasulfide), exhibits tetragonal symmetry and is a member of the stannite group that has the general formula A 2 BCX 4 , with A = Ag, Cu; B = Zn, Cd, Fe, Cu, Hg; C = Sn, Ge, Sb, As; and X = S, Se. In this study, single-crystal X-ray diffraction data are used to determine the structure of pirquitasite from a twinned crystal from the type locality, the Pirquitas deposit, Jujuy Province, Argentina, with anisotropic displacement parameters for all atoms, and a measured composition of (Ag 1.87 Cu 0.13 )(Zn 0.61 Fe 0.36 Cd 0.03 )SnS 4 . One Ag atom is located on Wyckoff site Wyckoff 2 a (symmetry -4..), the other Ag atom is statistically disordered with minor amounts of Cu and is located on 2 c (-4..), the (Zn, Fe, Cd) site on 2 d (-4..), Sn on 2 b (-4..), and S on general site 8 g . This is the first determination of the crystal structure of pirquitasite, and our data indicate that the space group of pirquitasite is I -4, rather than I -42 m as previously suggested. The structure was refined under consideration of twinning by inversion [twin ratio of the components 0.91 (6):0.09 (6)].
Benjamin N. SchumerRobert T. DownsKenneth J. DomanikMarcelo B. AndradeMarcus J. Origlieri
Tim KüllmeyJakob HeinEva M. HeppkeIlias EfthimiopoulosBeate Paulus
Francisco Yarur VillanuevaMinhal HashamPhilippe B. GreenChristian J. ImperialeSamihat RahmanDarcy C. BurnsMark W. B. Wilson
O. I. HuzenkoOleksandr DobrozhanД. И. КурбатовAnatoliy Opanasyuk
Weiyan GongTakahiro TabataKoji TakeiMasaru MorihamaTsuyoshi MaedaTakahiro Wada