Magnesioferrite Antao S M, Hassan I, Crichton W A, Parise J B American Mineralogist 90 (2005) 1500-1505 Effects of high pressure and high temperature on cation ordering in magnesioferrite, MgFe2O4, using in situ synchrotron X-ray powder diffraction up to 1430 K and 6 GPa Sample: T = 1030 K, P = 3 GPa during cooling _database_code_amcsd 0003921 CELL PARAMETERS: 8.4103 8.4103 8.4103 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 594.893 Density (g/cm3): 4.465 MAX. ABS. INTENSITY / VOLUME**2: 60.70933101 RIR: 4.427 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.27 5.54 4.8557 1 1 1 8 30.05 34.06 2.9735 2 2 0 12 35.40 100.00 2.5358 3 1 1 24 37.03 3.24 2.4279 2 2 2 8 43.02 20.63 2.1026 4 0 0 6 53.37 11.46 1.7168 4 2 2 24 56.89 28.24 1.6186 5 1 1 24 56.89 5.64 1.6186 3 3 3 8 62.47 45.64 1.4868 4 4 0 12 70.86 4.18 1.3298 6 2 0 24 73.89 8.98 1.2826 5 3 3 24 74.89 2.41 1.2679 6 2 2 24 78.85 2.41 1.2139 4 4 4 8 86.62 4.96 1.1239 6 4 2 48 89.51 8.08 1.0949 7 3 1 48 89.51 6.09 1.0949 5 5 3 24 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.