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 = 1090 K, P = 3 GPa during heating _database_code_amcsd 0003912 CELL PARAMETERS: 8.4101 8.4101 8.4101 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 594.849 Density (g/cm3): 4.466 MAX. ABS. INTENSITY / VOLUME**2: 59.06269631 RIR: 4.307 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.27 4.73 4.8556 1 1 1 8 30.05 33.89 2.9734 2 2 0 12 35.40 100.00 2.5357 3 1 1 24 37.03 3.23 2.4278 2 2 2 8 43.02 20.42 2.1025 4 0 0 6 53.37 10.76 1.7167 4 2 2 24 56.89 25.61 1.6185 5 1 1 24 56.89 5.64 1.6185 3 3 3 8 62.47 42.47 1.4867 4 4 0 12 70.87 3.69 1.3298 6 2 0 24 73.90 8.03 1.2825 5 3 3 24 74.90 2.28 1.2679 6 2 2 24 78.85 2.29 1.2139 4 4 4 8 86.62 3.95 1.1238 6 4 2 48 89.51 7.17 1.0949 7 3 1 48 89.51 5.00 1.0949 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.