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 = 1210 K, P = 3 GPa during cooling _database_code_amcsd 0003918 CELL PARAMETERS: 8.4333 8.4333 8.4333 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 599.783 Density (g/cm3): 4.429 MAX. ABS. INTENSITY / VOLUME**2: 56.82298958 RIR: 4.178 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.22 6.39 4.8690 1 1 1 8 29.97 31.44 2.9816 2 2 0 12 35.30 100.00 2.5427 3 1 1 24 36.92 4.96 2.4345 2 2 2 8 42.90 19.84 2.1083 4 0 0 6 53.21 9.71 1.7214 4 2 2 24 56.72 23.58 1.6230 5 1 1 24 56.72 5.78 1.6230 3 3 3 8 62.28 37.20 1.4908 4 4 0 12 70.64 3.24 1.3334 6 2 0 24 73.66 7.48 1.2861 5 3 3 24 74.65 3.51 1.2714 6 2 2 24 78.59 1.79 1.2172 4 4 4 8 86.33 3.24 1.1269 6 4 2 48 89.20 6.89 1.0979 7 3 1 48 89.20 4.23 1.0979 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.