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 = 500 C Note: P = 101 kPa _database_code_amcsd 0017859 CELL PARAMETERS: 4.9775 4.9775 17.3105 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 371.418 Density (g/cm3): 2.684 MAX. ABS. INTENSITY / VOLUME**2: 24.59620155 RIR: 2.983 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.05 8.09 3.8586 0 1 2 6 29.24 100.00 3.0541 1 0 4 6 31.00 1.70 2.8851 0 0 6 2 36.09 14.09 2.4887 1 1 0 6 39.43 14.87 2.2852 1 1 3 12 43.26 13.09 2.0915 2 0 2 6 46.99 17.32 1.9338 0 1 8 6 47.10 5.65 1.9293 0 2 4 6 48.30 17.35 1.8845 1 1 6 12 56.75 2.36 1.6221 2 1 1 12 57.56 7.97 1.6011 1 2 2 12 60.64 2.07 1.5270 2 0 8 6 60.74 4.18 1.5248 2 1 4 12 60.87 1.69 1.5219 1 1 9 12 63.06 1.30 1.4742 1 2 5 12 64.61 2.58 1.4425 0 0 12 2 64.89 4.13 1.4369 3 0 0 6 69.67 1.69 1.3496 0 2 10 6 72.64 1.97 1.3016 1 2 8 12 76.30 1.57 1.2480 1 1 12 12 81.05 1.69 1.1864 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.