#------------------------------------------------------------------------------ #$Date: 2013-05-05 17:21:46 +0300 (Sun, 05 May 2013) $ #$Revision: 85285 $ #$URL: file:///home/coder/svn-repositories/cod/cif/9/01/37/9013732.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_9013732 loop_ _publ_author_name 'Drits, V. A.' 'Zviagina, B. B.' 'McCarty, D. K.' 'Salyn, A. L.' _publ_section_title ; Factors responsible for crystal-chemical variations in the solid solutions from illite to aluminoceladonite and from glauconite to celadonite Locality: Athabasca basement; Saskatchewan, Canada Sample Name: 10564 ; _journal_name_full 'American Mineralogist' _journal_page_first 348 _journal_page_last 361 _journal_volume 95 _journal_year 2010 _chemical_formula_sum 'Al2 H2 K O12 Si4' _chemical_name_mineral Illite _space_group_IT_number 5 _symmetry_space_group_name_Hall 'C 2y' _symmetry_space_group_name_H-M 'C 1 2 1' _cell_angle_alpha 90 _cell_angle_beta 99.00 _cell_angle_gamma 90 _cell_length_a 5.1973 _cell_length_b 8.999 _cell_length_c 10.147 _cell_volume 468.737 _exptl_crystal_density_diffrn 2.830 _[local]_cod_chemical_formula_sum_orig 'K Al2 Si4 O12 H2' _cod_database_code 9013732 loop_ _symmetry_equiv_pos_as_xyz x,y,z 1/2+x,1/2+y,z -x,y,-z 1/2-x,1/2+y,-z loop_ _atom_site_label _atom_site_fract_x _atom_site_fract_y _atom_site_fract_z K 0.50000 0.65280 0.50000 Al1 0.50000 0.16670 0.00000 Al2 0.00000 0.33330 0.00000 Si1 0.43330 0.99210 0.26920 Si2 0.91850 0.82050 0.26920 O1 0.41520 0.99860 0.10630 O2 0.34320 0.30790 0.10630 O3 0.99580 0.65710 0.33430 O4 0.15850 0.93710 0.31290 O5 0.66960 0.88170 0.33430 O-H 0.84080 0.19000 0.10080