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 = 477 C Note: P = 101 kPa _database_code_amcsd 0017858 CELL PARAMETERS: 4.9775 4.9775 17.2949 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 371.083 Density (g/cm3): 2.687 MAX. ABS. INTENSITY / VOLUME**2: 24.91701289 RIR: 3.020 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.05 8.20 3.8579 0 1 2 6 29.26 100.00 3.0527 1 0 4 6 31.03 1.72 2.8825 0 0 6 2 36.09 14.16 2.4887 1 1 0 6 39.44 15.28 2.2849 1 1 3 12 43.26 13.38 2.0913 2 0 2 6 47.02 17.72 1.9325 0 1 8 6 47.11 5.80 1.9289 0 2 4 6 48.31 17.92 1.8838 1 1 6 12 56.75 2.46 1.6221 2 1 1 12 57.57 8.31 1.6011 1 2 2 12 60.67 2.17 1.5263 2 0 8 6 60.75 4.41 1.5246 2 1 4 12 60.91 1.80 1.5210 1 1 9 12 63.07 1.37 1.4739 1 2 5 12 64.67 2.74 1.4412 0 0 12 2 64.89 4.43 1.4369 3 0 0 6 69.71 1.80 1.3489 0 2 10 6 72.67 2.13 1.3011 1 2 8 12 76.36 1.68 1.2472 1 1 12 12 81.09 1.84 1.1859 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.