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 = 599 C Note: P = 101 kPa _database_code_amcsd 0017864 CELL PARAMETERS: 4.9766 4.9766 17.3757 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 372.682 Density (g/cm3): 2.675 MAX. ABS. INTENSITY / VOLUME**2: 23.94265679 RIR: 2.914 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.04 8.00 3.8609 0 1 2 6 29.19 100.00 3.0595 1 0 4 6 30.88 1.58 2.8960 0 0 6 2 36.10 14.09 2.4883 1 1 0 6 39.41 13.73 2.2862 1 1 3 12 43.26 12.58 2.0916 2 0 2 6 46.84 16.61 1.9396 0 1 8 6 47.07 5.45 1.9304 0 2 4 6 48.22 16.37 1.8873 1 1 6 12 56.76 2.07 1.6219 2 1 1 12 57.57 7.41 1.6011 1 2 2 12 60.52 1.93 1.5298 2 0 8 6 60.72 1.42 1.5253 1 1 9 12 60.72 3.84 1.5253 2 1 4 12 63.02 1.11 1.4750 1 2 5 12 64.34 2.29 1.4480 0 0 12 2 64.91 3.56 1.4366 3 0 0 6 69.49 1.51 1.3526 0 2 10 6 72.54 1.76 1.3032 1 2 8 12 76.05 1.41 1.2515 1 1 12 12 80.89 1.46 1.1884 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.