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 = 730 K, P = 3 GPa during heating _database_code_amcsd 0003908 CELL PARAMETERS: 8.3674 8.3674 8.3674 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 585.832 Density (g/cm3): 4.534 MAX. ABS. INTENSITY / VOLUME**2: 63.69297713 RIR: 4.574 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.37 2.80 4.8309 1 1 1 8 30.21 36.31 2.9583 2 2 0 12 35.59 100.00 2.5229 3 1 1 24 37.22 2.56 2.4155 2 2 2 8 43.25 19.15 2.0919 4 0 0 6 53.66 12.15 1.7080 4 2 2 24 57.21 27.85 1.6103 5 1 1 24 57.21 5.92 1.6103 3 3 3 8 62.82 46.77 1.4792 4 4 0 12 71.28 4.41 1.3230 6 2 0 24 74.34 9.24 1.2760 5 3 3 24 75.34 2.23 1.2614 6 2 2 24 79.33 2.60 1.2077 4 4 4 8 87.18 5.10 1.1181 6 4 2 48 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.