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 = 379 C Note: P = 101 kPa _database_code_amcsd 0017853 CELL PARAMETERS: 4.9740 4.9740 17.2510 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 369.621 Density (g/cm3): 2.697 MAX. ABS. INTENSITY / VOLUME**2: 24.39704887 RIR: 2.945 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.08 12.46 3.8538 0 1 2 6 29.30 100.00 3.0478 1 0 4 6 31.11 1.27 2.8752 0 0 6 2 36.12 15.10 2.4870 1 1 0 6 39.48 16.55 2.2827 1 1 3 12 43.30 15.25 2.0896 2 0 2 6 47.13 18.82 1.9283 0 1 8 6 47.17 7.33 1.9269 0 2 4 6 48.39 22.31 1.8810 1 1 6 12 56.80 1.98 1.6209 2 1 1 12 57.55 1.80 1.6015 1 0 10 6 57.61 9.91 1.5999 1 2 2 12 60.78 3.03 1.5239 2 0 8 6 60.81 6.49 1.5232 2 1 4 12 61.03 1.82 1.5182 1 1 9 12 63.14 1.08 1.4724 1 2 5 12 64.86 3.06 1.4376 0 0 12 2 64.95 5.99 1.4359 3 0 0 6 69.86 2.46 1.3464 0 2 10 6 72.78 3.41 1.2994 1 2 8 12 76.55 2.56 1.2446 1 1 12 12 81.25 2.69 1.1841 2 1 10 12 84.07 1.26 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.