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 = 337 C Note: P = 101 kPa _database_code_amcsd 0017851 CELL PARAMETERS: 4.9760 4.9760 17.2270 90.000 90.000 120.000 SPACE GROUP: R-3c X-RAY WAVELENGTH: 1.541838 Cell Volume: 369.403 Density (g/cm3): 2.699 MAX. ABS. INTENSITY / VOLUME**2: 24.75288429 RIR: 2.986 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 23.08 12.85 3.8539 0 1 2 6 29.32 100.00 3.0462 1 0 4 6 31.15 1.12 2.8712 0 0 6 2 36.10 15.64 2.4880 1 1 0 6 39.47 16.22 2.2829 1 1 3 12 43.29 15.81 2.0903 2 0 2 6 47.17 7.78 1.9270 0 2 4 6 47.18 19.28 1.9263 0 1 8 6 48.41 23.27 1.8803 1 1 6 12 56.77 1.93 1.6215 2 1 1 12 57.59 10.68 1.6004 1 2 2 12 57.62 2.06 1.5996 1 0 10 6 60.80 7.14 1.5235 2 1 4 12 60.81 3.34 1.5231 2 0 8 6 61.08 1.76 1.5171 1 1 9 12 63.14 1.04 1.4725 1 2 5 12 64.92 6.37 1.4364 3 0 0 6 64.96 3.18 1.4356 0 0 12 2 69.91 2.73 1.3455 0 2 10 6 72.81 3.89 1.2990 1 2 8 12 76.63 2.99 1.2434 1 1 12 12 81.29 3.12 1.1835 2 1 10 12 84.04 1.42 1.1517 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.