#------------------------------------------------------------------------------ #$Date: 2016-02-16 14:49:47 +0200 (Tue, 16 Feb 2016) $ #$Revision: 176465 $ #$URL: file:///home/coder/svn-repositories/cod/cif/9/01/55/9015593.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_9015593 loop_ _publ_author_name 'Antao, S. M.' 'Hassan, I.' _publ_section_title ; Temperature dependence of the structural parameters in the transformation of aragonite to calcite, as determined from in situ synchrotron powder X-ray-diffraction data Note: T = 318 C Note: P = 101 kPa ; _journal_name_full 'The Canadian Mineralogist' _journal_page_first 1225 _journal_page_last 1236 _journal_paper_doi 10.3749/canmin.48.5.1225 _journal_volume 48 _journal_year 2010 _chemical_compound_source 'Cuenca, Spain' _chemical_formula_sum 'C Ca O3' _chemical_name_mineral Aragonite _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 4.9693 _cell_length_b 8.0234 _cell_length_c 5.8037 _cell_volume 231.397 _database_code_amcsd 0017840 _exptl_crystal_density_diffrn 2.873 _cod_original_formula_sum 'Ca C O3' _cod_database_code 9015593 loop_ _space_group_symop_operation_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_U_iso_or_equiv Ca 0.25000 0.41320 0.75520 0.01700 C 0.25000 0.76280 -0.06330 0.03600 O1 0.25000 0.91980 -0.08520 0.03600 O2 0.47190 0.68600 -0.09780 0.03600