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 = 1430 K, P = 3 GPa during heating _database_code_amcsd 0003916 CELL PARAMETERS: 8.4479 8.4479 8.4479 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 602.893 Density (g/cm3): 4.406 MAX. ABS. INTENSITY / VOLUME**2: 56.09593671 RIR: 4.146 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.19 8.00 4.8774 1 1 1 8 29.92 30.11 2.9868 2 2 0 12 35.24 100.00 2.5471 3 1 1 24 36.86 4.30 2.4387 2 2 2 8 42.82 22.10 2.1120 4 0 0 6 53.11 9.75 1.7244 4 2 2 24 56.61 23.85 1.6258 5 1 1 24 56.61 5.73 1.6258 3 3 3 8 62.16 39.87 1.4934 4 4 0 12 70.50 3.39 1.3357 6 2 0 24 73.51 7.51 1.2883 5 3 3 24 74.50 2.47 1.2736 6 2 2 24 78.43 2.00 1.2193 4 4 4 8 86.14 3.54 1.1289 6 4 2 48 89.01 6.76 1.0998 7 3 1 48 89.01 4.34 1.0998 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.