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 = 1130 K, P = 3 GPa during cooling _database_code_amcsd 0003919 CELL PARAMETERS: 8.4248 8.4248 8.4248 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 597.978 Density (g/cm3): 4.442 MAX. ABS. INTENSITY / VOLUME**2: 58.45859859 RIR: 4.285 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.24 6.88 4.8641 1 1 1 8 30.00 32.10 2.9786 2 2 0 12 35.33 100.00 2.5402 3 1 1 24 36.96 4.33 2.4320 2 2 2 8 42.94 20.02 2.1062 4 0 0 6 53.27 10.71 1.7197 4 2 2 24 56.78 25.79 1.6214 5 1 1 24 56.78 5.77 1.6214 3 3 3 8 62.35 40.61 1.4893 4 4 0 12 70.72 3.87 1.3321 6 2 0 24 73.75 8.25 1.2848 5 3 3 24 74.74 3.01 1.2701 6 2 2 24 78.69 1.81 1.2160 4 4 4 8 86.43 4.32 1.1258 6 4 2 48 89.31 5.07 1.0968 5 5 3 24 89.31 7.65 1.0968 7 3 1 48 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.