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 = 420 C Note: P = 101 kPa _database_code_amcsd 0017855 CELL PARAMETERS: 4.9748 4.9748 17.2700 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 370.147 Density (g/cm3): 2.694 MAX. ABS. INTENSITY / VOLUME**2: 24.47089557 RIR: 2.958 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.07 11.17 3.8551 0 1 2 6 29.29 100.00 3.0497 1 0 4 6 31.07 1.48 2.8783 0 0 6 2 36.11 14.60 2.4874 1 1 0 6 39.46 16.62 2.2834 1 1 3 12 43.29 14.65 2.0901 2 0 2 6 47.09 18.49 1.9300 0 1 8 6 47.15 6.78 1.9276 0 2 4 6 48.36 21.01 1.8820 1 1 6 12 56.79 2.17 1.6212 2 1 1 12 57.49 1.49 1.6030 1 0 10 6 57.60 9.29 1.6002 1 2 2 12 60.74 2.71 1.5248 2 0 8 6 60.79 5.76 1.5236 2 1 4 12 60.98 1.91 1.5193 1 1 9 12 63.12 1.20 1.4729 1 2 5 12 64.78 3.00 1.4392 0 0 12 2 64.93 5.57 1.4361 3 0 0 6 69.80 2.22 1.3474 0 2 10 6 72.74 2.94 1.3000 1 2 8 12 76.47 2.20 1.2457 1 1 12 12 81.19 2.35 1.1848 2 1 10 12 84.05 1.14 1.1516 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.