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 = 297 C Note: P = 101 kPa _database_code_amcsd 0017849 CELL PARAMETERS: 4.9800 4.9800 17.1920 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 369.246 Density (g/cm3): 2.700 MAX. ABS. INTENSITY / VOLUME**2: 24.56667779 RIR: 2.962 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.07 13.25 3.8548 0 1 2 6 29.34 100.00 3.0444 1 0 4 6 36.07 16.27 2.4900 1 1 0 6 39.46 15.03 2.2837 1 1 3 12 43.26 16.00 2.0916 2 0 2 6 47.15 8.02 1.9274 0 2 4 6 47.26 18.98 1.9234 0 1 8 6 48.43 23.21 1.8795 1 1 6 12 56.73 1.71 1.6228 2 1 1 12 57.55 10.94 1.6015 1 2 2 12 57.73 2.27 1.5970 1 0 10 6 60.77 7.36 1.5242 2 1 4 12 60.86 3.47 1.5222 2 0 8 6 61.15 1.47 1.5156 1 1 9 12 64.86 6.13 1.4376 3 0 0 6 65.11 2.96 1.4327 0 0 12 2 69.99 2.77 1.3443 0 2 10 6 72.82 4.03 1.2987 1 2 8 12 76.75 3.16 1.2418 1 1 12 12 81.34 3.21 1.1829 2 1 10 12 83.98 1.39 1.1524 1 3 4 12 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.