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 = 1220 K, P = 3 GPa during heating _database_code_amcsd 0003914 CELL PARAMETERS: 8.4233 8.4233 8.4233 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 597.652 Density (g/cm3): 4.445 MAX. ABS. INTENSITY / VOLUME**2: 58.68145149 RIR: 4.299 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.24 5.41 4.8632 1 1 1 8 30.01 32.33 2.9781 2 2 0 12 35.34 100.00 2.5397 3 1 1 24 36.97 3.39 2.4316 2 2 2 8 42.95 21.19 2.1058 4 0 0 6 53.28 10.61 1.7194 4 2 2 24 56.79 24.89 1.6211 5 1 1 24 56.79 5.85 1.6211 3 3 3 8 62.36 42.62 1.4890 4 4 0 12 70.74 3.75 1.3318 6 2 0 24 73.76 8.04 1.2845 5 3 3 24 74.76 2.16 1.2699 6 2 2 24 78.70 2.26 1.2158 4 4 4 8 86.45 4.02 1.1256 6 4 2 48 89.34 4.89 1.0966 5 5 3 24 89.34 7.38 1.0966 7 3 1 48 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.