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 = 620 K, P = 5 GPa during cooling _database_code_amcsd 0003907 CELL PARAMETERS: 8.3332 8.3332 8.3332 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 578.674 Density (g/cm3): 4.590 MAX. ABS. INTENSITY / VOLUME**2: 64.70547247 RIR: 4.590 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.44 2.64 4.8112 1 1 1 8 30.34 37.20 2.9462 2 2 0 12 35.74 100.00 2.5126 3 1 1 24 37.38 2.48 2.4056 2 2 2 8 43.44 19.06 2.0833 4 0 0 6 53.90 12.16 1.7010 4 2 2 24 57.46 5.74 1.6037 3 3 3 8 57.46 28.68 1.6037 5 1 1 24 63.11 47.30 1.4731 4 4 0 12 71.62 4.33 1.3176 6 2 0 24 74.69 9.34 1.2708 5 3 3 24 75.71 2.32 1.2563 6 2 2 24 79.72 2.78 1.2028 4 4 4 8 87.62 5.06 1.1136 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.