Acta Cryst. (2006). B62, 447-456 [ doi:10.1107/S010876810600975X ]
Abstract: The crystal structures of 222- and 221-polybasite [(Ag,Cu)16(Sb,As)2S11] crystals have been solved and refined by means of X-ray diffraction data (collected at 100 and 120 K, respectively) from twinned crystals. Both structures consist of the stacking of [(Ag,Cu)6Sb2S7]2- and [Ag9CuS4]2+ module layers in which Sb forms isolated SbS3 pyramids typically occurring in sulfosalts; copper links two S atoms in a linear coordination and silver occupies sites with coordination ranging from quasi-linear to almost tetrahedral. An Ag
Cu substitution in the [(Ag,Cu)6Sb2S7]2- module layer is observed in both structures, the substitution amount being larger in the 221- than in the 222-polybasite. A pattern of the possible mechanism regulating the type of unit cell that is stabilized is proposed: starting from the hypothetical stoichiometric and fully ordered Ag15CuSb2S11 222-polybasite structure, with a low C2/c monoclinic symmetry and a large 222 supercell, the disorder introduced by the substitution of Cu for Ag increases the symmetry with a cell reduction along the c axis yielding the 221 supercell and a trigonal crystal system. A further increase of the substitution gives rise to a folding of the cell along the a and b axes and the 111-pearceite structure, space group
.
Keywords: polybasite; crystal X-ray structure determination; twin; polytype; disorder.
![]() ![]() Structure factor file (CIF format) (321.4 kbytes) | |
![]() ![]() Structure factor file (CIF format) (2054.1 kbytes) | |
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