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 = 970 K, P = 6 GPa during cooling _database_code_amcsd 0003897 CELL PARAMETERS: 8.3453 8.3453 8.3453 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 581.202 Density (g/cm3): 4.570 MAX. ABS. INTENSITY / VOLUME**2: 62.16495099 RIR: 4.429 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.41 3.07 4.8182 1 1 1 8 30.29 37.22 2.9505 2 2 0 12 35.68 100.00 2.5162 3 1 1 24 37.33 2.54 2.4091 2 2 2 8 43.37 18.76 2.0863 4 0 0 6 53.82 11.80 1.7035 4 2 2 24 57.37 5.47 1.6061 3 3 3 8 57.37 27.44 1.6061 5 1 1 24 63.01 44.28 1.4753 4 4 0 12 71.50 4.07 1.3195 6 2 0 24 74.57 8.50 1.2726 5 3 3 24 75.58 2.05 1.2581 6 2 2 24 79.59 2.34 1.2045 4 4 4 8 87.46 4.62 1.1152 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.