#------------------------------------------------------------------------------ #$Date: 2010-06-10 18:11:07 +0300 (Thu, 10 Jun 2010) $ #$Revision: 1210 $ #$URL: file:///home/coder/svn-repositories/cod/cif/9/9003569.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_9003569 loop_ _publ_author_name 'Crichton, W. A.' 'Parise, J. B.' 'Antao, S. M.' 'Grzechnik, A.' _publ_section_title ; Evidence for monazite-, barite-, and AgMnO4 (distorted barite)-type structures of CaSO4 at high pressure and temperature Sample: P = 21 GPa, T = 1450 K ; _journal_name_full 'American Mineralogist' _journal_page_first 22 _journal_page_last 27 _journal_volume 90 _journal_year 2005 _chemical_formula_sum 'Ca O4 S' _chemical_name_mineral CaSO4 _space_group_IT_number 62 _symmetry_space_group_name_Hall '-P 2c 2ab' _symmetry_space_group_name_H-M 'P b n m' _cell_angle_alpha 90 _cell_angle_beta 90 _cell_angle_gamma 90 _cell_length_a 6.3365 _cell_length_b 7.5347 _cell_length_c 4.9532 _cell_volume 236.484 _diffrn_ambient_pressure 2.1e+07 _diffrn_ambient_temperature 1450 _exptl_crystal_density_diffrn 3.824 _[local]_cod_chemical_formula_sum_orig 'Ca S O4' _cod_database_code 9003569 _amcsd_database_code AMCSD#0003661 loop_ _symmetry_equiv_pos_as_xyz x,y,z x,y,1/2-z -x,-y,1/2+z 1/2+x,1/2-y,1/2+z 1/2-x,1/2+y,1/2-z 1/2-x,1/2+y,z 1/2+x,1/2-y,-z -x,-y,-z loop_ _atom_site_label _atom_site_fract_x _atom_site_fract_y _atom_site_fract_z _atom_site_U_iso_or_equiv Ca 0.16960 0.18120 0.25000 0.02980 S 0.81660 0.56060 0.25000 0.04520 O1 0.56750 0.88980 0.25000 0.03340 O2 0.53410 0.21410 0.25000 0.03340 O3 0.31930 0.42870 0.98230 0.03340