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 = 860 K, P = 6 GPa during cooling _database_code_amcsd 0003898 CELL PARAMETERS: 8.3363 8.3363 8.3363 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 579.322 Density (g/cm3): 4.585 MAX. ABS. INTENSITY / VOLUME**2: 63.17112800 RIR: 4.486 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.43 2.50 4.8130 1 1 1 8 30.33 38.08 2.9473 2 2 0 12 35.72 100.00 2.5135 3 1 1 24 37.37 2.38 2.4065 2 2 2 8 43.42 18.26 2.0841 4 0 0 6 53.88 12.13 1.7016 4 2 2 24 57.44 5.52 1.6043 3 3 3 8 57.44 27.85 1.6043 5 1 1 24 63.09 44.93 1.4737 4 4 0 12 71.59 4.21 1.3181 6 2 0 24 74.66 8.72 1.2713 5 3 3 24 75.68 2.07 1.2567 6 2 2 24 79.69 2.39 1.2032 4 4 4 8 87.58 4.81 1.1140 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.