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 = 398 C Note: P = 101 kPa _database_code_amcsd 0017854 CELL PARAMETERS: 4.9740 4.9740 17.2610 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 369.835 Density (g/cm3): 2.696 MAX. ABS. INTENSITY / VOLUME**2: 24.54634518 RIR: 2.965 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.08 11.89 3.8542 0 1 2 6 29.30 100.00 3.0486 1 0 4 6 31.09 1.34 2.8768 0 0 6 2 36.12 14.96 2.4870 1 1 0 6 39.47 16.51 2.2829 1 1 3 12 43.30 15.08 2.0897 2 0 2 6 47.11 18.80 1.9292 0 1 8 6 47.16 7.16 1.9271 0 2 4 6 48.38 21.90 1.8814 1 1 6 12 56.80 2.06 1.6209 2 1 1 12 57.52 1.70 1.6023 1 0 10 6 57.61 9.78 1.5999 1 2 2 12 60.76 2.94 1.5243 2 0 8 6 60.81 6.27 1.5233 2 1 4 12 61.01 1.85 1.5187 1 1 9 12 63.14 1.13 1.4726 1 2 5 12 64.82 3.07 1.4384 0 0 12 2 64.95 5.87 1.4359 3 0 0 6 69.83 2.41 1.3469 0 2 10 6 72.77 3.28 1.2996 1 2 8 12 76.51 2.48 1.2452 1 1 12 12 81.22 2.61 1.1844 2 1 10 12 84.06 1.23 1.1514 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.