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 = 1130 K, P = 5 GPa during heating _database_code_amcsd 0003904 CELL PARAMETERS: 8.3730 8.3730 8.3730 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 587.015 Density (g/cm3): 4.525 MAX. ABS. INTENSITY / VOLUME**2: 60.98570578 RIR: 4.388 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.35 3.23 4.8342 1 1 1 8 30.19 35.44 2.9603 2 2 0 12 35.56 100.00 2.5246 3 1 1 24 37.20 2.88 2.4171 2 2 2 8 43.22 19.17 2.0933 4 0 0 6 53.62 11.27 1.7091 4 2 2 24 57.16 25.58 1.6114 5 1 1 24 57.16 5.76 1.6114 3 3 3 8 62.78 42.69 1.4802 4 4 0 12 71.23 3.88 1.3239 6 2 0 24 74.28 8.20 1.2769 5 3 3 24 75.29 2.22 1.2623 6 2 2 24 79.27 2.25 1.2085 4 4 4 8 87.10 4.16 1.1189 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.