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 = 890 K, P = 3 GPa during cooling _database_code_amcsd 0003922 CELL PARAMETERS: 8.3989 8.3989 8.3989 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 592.465 Density (g/cm3): 4.484 MAX. ABS. INTENSITY / VOLUME**2: 61.85848577 RIR: 4.492 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.30 4.56 4.8491 1 1 1 8 30.09 34.05 2.9694 2 2 0 12 35.45 100.00 2.5324 3 1 1 24 37.08 3.09 2.4245 2 2 2 8 43.08 20.17 2.0997 4 0 0 6 53.44 11.73 1.7144 4 2 2 24 56.97 27.51 1.6164 5 1 1 24 56.97 5.94 1.6164 3 3 3 8 62.56 45.88 1.4847 4 4 0 12 70.97 4.38 1.3280 6 2 0 24 74.01 9.11 1.2808 5 3 3 24 75.01 2.33 1.2662 6 2 2 24 78.98 2.38 1.2123 4 4 4 8 86.77 5.13 1.1223 6 4 2 48 89.67 8.60 1.0934 7 3 1 48 89.67 6.10 1.0934 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.