#------------------------------------------------------------------------------ #$Date: 2013-05-05 17:21:46 +0300 (Sun, 05 May 2013) $ #$Revision: 85285 $ #$URL: file:///home/coder/svn-repositories/cod/cif/9/01/05/9010571.cif $ #------------------------------------------------------------------------------ # # This file is available in the Crystallography Open Database (COD), # http://www.crystallography.net/. The original data for this entry # were provided the American Mineralogist Crystal Structure Database, # http://rruff.geo.arizona.edu/AMS/amcsd.php # # The file may be used within the scientific community so long as # proper attribution is given to the journal article from which the # data were obtained. # data_9010571 loop_ _publ_author_name 'Petricek, V.' 'Makovicky, E.' _publ_section_title ;Interpretation of selected structures of the bismuthinite - aikinite series as commensurately modulated structures Locality: synthetic Sample: oversubstituted gladite ; _journal_name_full 'The Canadian Mineralogist' _journal_page_first 189 _journal_page_last 206 _journal_volume 44 _journal_year 2006 _chemical_formula_sum 'Bi1.602 Cu0.388 Pb0.398 S3' _chemical_name_mineral Gladite _space_group_IT_number 62 _symmetry_space_group_name_Hall '-P 2n 2a' _symmetry_space_group_name_H-M 'P m c n' _cell_angle_alpha 90 _cell_angle_beta 90 _cell_angle_gamma 90 _cell_length_a 4.0100 _cell_length_b 11.1963 _cell_length_c 11.502 _cell_volume 516.407 _exptl_crystal_density_diffrn 6.921 _[local]_cod_chemical_formula_sum_orig 'Cu.388 Pb.398 Bi1.602 S3' _cod_database_code 9010571 loop_ _symmetry_equiv_pos_as_xyz x,y,z 1/2-x,y,z 1/2+x,-y,-z 1/2+x,1/2+y,1/2-z 1/2-x,1/2-y,1/2+z x,1/2-y,1/2+z -x,1/2+y,1/2-z -x,-y,-z loop_ _atom_site_label _atom_site_fract_x _atom_site_fract_y _atom_site_fract_z _atom_site_occupancy _atom_site_U_iso_or_equiv Cu1 0.25000 0.71410 0.72060 0.25000 0.04260 Cu2 0.25000 0.70570 0.73240 0.13800 0.04000 PbM2 0.25000 0.52284 0.33716 0.39750 0.04163 BiM2 0.25000 0.52284 0.33716 0.60250 0.04163 BiM1 0.25000 0.17793 0.51838 1.00000 0.03650 S1 0.25000 -0.05630 0.37820 1.00000 0.03300 S2 0.25000 0.63170 0.54730 1.00000 0.03440 S3 0.25000 0.30520 0.71580 1.00000 0.03240