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 = 556 C Note: P = 101 kPa _database_code_amcsd 0017862 CELL PARAMETERS: 4.9769 4.9769 17.3479 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 372.131 Density (g/cm3): 2.679 MAX. ABS. INTENSITY / VOLUME**2: 24.07307943 RIR: 2.926 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.04 8.07 3.8599 0 1 2 6 29.21 100.00 3.0572 1 0 4 6 30.93 1.62 2.8913 0 0 6 2 36.09 14.06 2.4885 1 1 0 6 39.42 14.13 2.2858 1 1 3 12 43.26 12.71 2.0915 2 0 2 6 46.90 16.76 1.9371 0 1 8 6 47.09 5.49 1.9299 0 2 4 6 48.25 16.63 1.8861 1 1 6 12 56.76 2.15 1.6219 2 1 1 12 57.57 7.53 1.6011 1 2 2 12 60.57 1.96 1.5286 2 0 8 6 60.73 3.92 1.5250 2 1 4 12 60.78 1.50 1.5239 1 1 9 12 63.04 1.16 1.4746 1 2 5 12 64.45 2.36 1.4457 0 0 12 2 64.90 3.72 1.4367 3 0 0 6 69.57 1.55 1.3514 0 2 10 6 72.58 1.80 1.3025 1 2 8 12 76.15 1.44 1.2500 1 1 12 12 80.96 1.50 1.1875 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.