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 = 620 C Note: P = 101 kPa _database_code_amcsd 0017865 CELL PARAMETERS: 4.9764 4.9764 17.3886 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 372.929 Density (g/cm3): 2.674 MAX. ABS. INTENSITY / VOLUME**2: 23.77630971 RIR: 2.896 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.03 8.05 3.8613 0 1 2 6 29.18 100.00 3.0606 1 0 4 6 30.85 1.54 2.8981 0 0 6 2 36.10 14.12 2.4882 1 1 0 6 39.41 13.47 2.2864 1 1 3 12 43.26 12.49 2.0916 2 0 2 6 46.81 16.45 1.9407 0 1 8 6 47.07 5.43 1.9307 0 2 4 6 48.20 16.21 1.8879 1 1 6 12 56.76 1.99 1.6218 2 1 1 12 57.57 7.30 1.6011 1 2 2 12 60.50 1.92 1.5303 2 0 8 6 60.69 1.36 1.5260 1 1 9 12 60.72 3.79 1.5253 2 1 4 12 63.02 1.06 1.4751 1 2 5 12 64.28 2.22 1.4490 0 0 12 2 64.91 3.46 1.4366 3 0 0 6 69.46 1.48 1.3532 0 2 10 6 72.52 1.72 1.3035 1 2 8 12 76.00 1.39 1.2522 1 1 12 12 80.86 1.42 1.1888 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.