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 = 960 K, P = 3 GPa during heating _database_code_amcsd 0003910 CELL PARAMETERS: 8.3891 8.3891 8.3891 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 590.410 Density (g/cm3): 4.499 MAX. ABS. INTENSITY / VOLUME**2: 61.82986798 RIR: 4.475 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.32 2.67 4.8435 1 1 1 8 30.13 36.07 2.9660 2 2 0 12 35.49 100.00 2.5294 3 1 1 24 37.12 2.57 2.4217 2 2 2 8 43.13 19.14 2.0973 4 0 0 6 53.51 11.71 1.7124 4 2 2 24 57.04 26.32 1.6145 5 1 1 24 57.04 5.87 1.6145 3 3 3 8 62.64 44.69 1.4830 4 4 0 12 71.07 4.11 1.3264 6 2 0 24 74.11 8.60 1.2793 5 3 3 24 75.12 2.09 1.2647 6 2 2 24 79.09 2.45 1.2109 4 4 4 8 86.89 4.49 1.1210 6 4 2 48 89.80 7.97 1.0922 7 3 1 48 89.80 5.57 1.0922 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.