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 = 318 C Note: P = 101 kPa _database_code_amcsd 0017850 CELL PARAMETERS: 4.9780 4.9780 17.2110 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 369.357 Density (g/cm3): 2.699 MAX. ABS. INTENSITY / VOLUME**2: 24.47886130 RIR: 2.953 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.07 13.36 3.8544 0 1 2 6 29.33 100.00 3.0454 1 0 4 6 36.09 15.98 2.4890 1 1 0 6 39.46 15.57 2.2834 1 1 3 12 43.27 15.91 2.0909 2 0 2 6 47.16 7.94 1.9272 0 2 4 6 47.22 19.03 1.9250 0 1 8 6 48.42 23.29 1.8799 1 1 6 12 56.75 1.76 1.6222 2 1 1 12 57.57 10.76 1.6010 1 2 2 12 57.67 2.20 1.5984 1 0 10 6 60.78 7.27 1.5238 2 1 4 12 60.83 3.41 1.5227 2 0 8 6 61.11 1.57 1.5164 1 1 9 12 64.89 6.21 1.4370 3 0 0 6 65.03 3.02 1.4342 0 0 12 2 69.95 2.73 1.3450 0 2 10 6 72.81 3.96 1.2989 1 2 8 12 76.68 3.06 1.2427 1 1 12 12 81.31 3.13 1.1833 2 1 10 12 84.01 1.38 1.1520 1 3 4 12 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.