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 = 1150 K, P = 6 GPa during heating _database_code_amcsd 0003896 CELL PARAMETERS: 8.3549 8.3549 8.3549 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 583.208 Density (g/cm3): 4.555 MAX. ABS. INTENSITY / VOLUME**2: 61.31301202 RIR: 4.383 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.39 3.17 4.8237 1 1 1 8 30.26 36.60 2.9539 2 2 0 12 35.64 100.00 2.5191 3 1 1 24 37.28 2.62 2.4119 2 2 2 8 43.32 18.93 2.0887 4 0 0 6 53.75 11.54 1.7054 4 2 2 24 57.30 5.52 1.6079 3 3 3 8 57.30 26.50 1.6079 5 1 1 24 62.93 43.29 1.4770 4 4 0 12 71.40 3.95 1.3210 6 2 0 24 74.47 8.22 1.2741 5 3 3 24 75.48 2.01 1.2595 6 2 2 24 79.48 2.27 1.2059 4 4 4 8 87.34 4.35 1.1165 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.