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 = 644 C Note: P = 101 kPa _database_code_amcsd 0017866 CELL PARAMETERS: 4.9761 4.9761 17.4163 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 373.478 Density (g/cm3): 2.670 MAX. ABS. INTENSITY / VOLUME**2: 23.60659029 RIR: 2.879 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.03 7.98 3.8624 0 1 2 6 29.16 100.00 3.0629 1 0 4 6 30.80 1.49 2.9027 0 0 6 2 36.10 14.15 2.4880 1 1 0 6 39.40 13.02 2.2869 1 1 3 12 43.26 12.32 2.0916 2 0 2 6 46.75 16.25 1.9432 0 1 8 6 47.06 5.38 1.9312 0 2 4 6 48.17 15.90 1.8891 1 1 6 12 56.77 1.90 1.6217 2 1 1 12 57.57 7.15 1.6010 1 2 2 12 60.45 1.88 1.5314 2 0 8 6 60.62 1.27 1.5275 1 1 9 12 60.71 3.70 1.5256 2 1 4 12 64.17 2.14 1.4514 0 0 12 2 64.91 3.28 1.4365 3 0 0 6 69.38 1.44 1.3545 0 2 10 6 72.47 1.67 1.3042 1 2 8 12 75.89 1.36 1.2537 1 1 12 12 80.79 1.36 1.1896 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.