Calcite Antao S M, Hassan I The Canadian Mineralogist 48 (2010) 1225-1236 Temperature dependence of the structural parameters in the transformation of aragonite to calcite, as determined from in situ synchrotron powder X-ray-diffraction data Locality: Cuenca, Spain Note: T = 540 C Note: P = 101 kPa _database_code_amcsd 0017861 CELL PARAMETERS: 4.9771 4.9771 17.3369 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 371.925 Density (g/cm3): 2.681 MAX. ABS. INTENSITY / VOLUME**2: 24.21347887 RIR: 2.941 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.04 8.04 3.8595 0 1 2 6 29.22 100.00 3.0563 1 0 4 6 30.95 1.65 2.8895 0 0 6 2 36.09 14.06 2.4885 1 1 0 6 39.42 14.30 2.2856 1 1 3 12 43.26 12.79 2.0915 2 0 2 6 46.93 16.88 1.9362 0 1 8 6 47.09 5.52 1.9297 0 2 4 6 48.26 16.77 1.8856 1 1 6 12 56.76 2.21 1.6220 2 1 1 12 57.57 7.63 1.6011 1 2 2 12 60.59 1.98 1.5281 2 0 8 6 60.73 3.97 1.5250 2 1 4 12 60.81 1.54 1.5233 1 1 9 12 63.05 1.19 1.4745 1 2 5 12 64.50 2.41 1.4447 0 0 12 2 64.90 3.80 1.4368 3 0 0 6 69.60 1.58 1.3509 0 2 10 6 72.60 1.83 1.3022 1 2 8 12 76.20 1.46 1.2494 1 1 12 12 80.99 1.54 1.1872 2 1 10 12 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.