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 = 1070 K, P = 3 GPa during cooling _database_code_amcsd 0003920 CELL PARAMETERS: 8.4180 8.4180 8.4180 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 596.518 Density (g/cm3): 4.453 MAX. ABS. INTENSITY / VOLUME**2: 59.51120288 RIR: 4.351 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.25 6.06 4.8601 1 1 1 8 30.02 33.37 2.9762 2 2 0 12 35.36 100.00 2.5381 3 1 1 24 36.99 3.80 2.4301 2 2 2 8 42.98 20.02 2.1045 4 0 0 6 53.31 11.10 1.7183 4 2 2 24 56.83 27.02 1.6200 5 1 1 24 56.83 5.68 1.6200 3 3 3 8 62.40 42.65 1.4881 4 4 0 12 70.79 4.01 1.3310 6 2 0 24 73.82 8.57 1.2837 5 3 3 24 74.81 2.80 1.2691 6 2 2 24 78.76 2.04 1.2150 4 4 4 8 86.52 4.59 1.1249 6 4 2 48 89.41 7.84 1.0959 7 3 1 48 89.41 5.52 1.0959 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.