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 = 1320 K, P = 3 GPa during cooling _database_code_amcsd 0003917 CELL PARAMETERS: 8.4404 8.4404 8.4404 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 601.306 Density (g/cm3): 4.418 MAX. ABS. INTENSITY / VOLUME**2: 56.57680360 RIR: 4.170 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.20 8.47 4.8731 1 1 1 8 29.94 29.80 2.9841 2 2 0 12 35.27 100.00 2.5449 3 1 1 24 36.89 4.82 2.4365 2 2 2 8 42.86 22.00 2.1101 4 0 0 6 53.16 9.59 1.7229 4 2 2 24 56.67 5.76 1.6244 3 3 3 8 56.67 24.24 1.6244 5 1 1 24 62.22 39.56 1.4921 4 4 0 12 70.57 3.33 1.3346 6 2 0 24 73.59 7.69 1.2872 5 3 3 24 74.58 3.04 1.2724 6 2 2 24 78.51 2.03 1.2183 4 4 4 8 86.24 3.49 1.1279 6 4 2 48 89.11 7.03 1.0989 7 3 1 48 89.11 4.48 1.0989 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.