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 = 434 C Note: P = 101 kPa _database_code_amcsd 0017856 CELL PARAMETERS: 4.9757 4.9757 17.2730 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 370.345 Density (g/cm3): 2.692 MAX. ABS. INTENSITY / VOLUME**2: 24.65496686 RIR: 2.982 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.07 10.21 3.8558 0 1 2 6 29.28 100.00 3.0502 1 0 4 6 31.07 1.57 2.8788 0 0 6 2 36.10 14.42 2.4878 1 1 0 6 39.46 16.38 2.2838 1 1 3 12 43.28 14.30 2.0905 2 0 2 6 47.08 18.31 1.9304 0 1 8 6 47.14 6.47 1.9279 0 2 4 6 48.35 20.13 1.8823 1 1 6 12 56.78 2.29 1.6215 2 1 1 12 57.48 1.31 1.6033 1 0 10 6 57.59 9.01 1.6005 1 2 2 12 60.73 2.54 1.5251 2 0 8 6 60.78 5.34 1.5239 2 1 4 12 60.97 1.91 1.5196 1 1 9 12 63.11 1.28 1.4732 1 2 5 12 64.77 2.95 1.4394 0 0 12 2 64.92 5.27 1.4364 3 0 0 6 69.78 2.10 1.3477 0 2 10 6 72.73 2.68 1.3002 1 2 8 12 76.45 2.03 1.2459 1 1 12 12 81.17 2.20 1.1850 2 1 10 12 84.03 1.07 1.1518 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.