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Pirquitasite, Ag(2)ZnSnS(4)

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 diffrac...

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Detalles Bibliográficos
Autores principales: Schumer, Benjamin N., Downs, Robert T., Domanik, Kenneth J., Andrade, Marcelo B, Origlieri, Marcus J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: International Union of Crystallography 2013
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3569172/
https://www.ncbi.nlm.nih.gov/pubmed/23424398
http://dx.doi.org/10.1107/S1600536813001013
Descripción
Sumario: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 2a (symmetry -4..), the other Ag atom is statistically disordered with minor amounts of Cu and is located on 2c (-4..), the (Zn, Fe, Cd) site on 2d (-4..), Sn on 2b (-4..), and S on general site 8g. 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-42m as previously suggested. The structure was refined under consideration of twinning by inversion [twin ratio of the components 0.91 (6):0.09 (6)].