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 = 1070 K, P = 5 GPa during heating _database_code_amcsd 0003903 CELL PARAMETERS: 8.3654 8.3654 8.3654 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 585.404 Density (g/cm3): 4.538 MAX. ABS. INTENSITY / VOLUME**2: 61.58225995 RIR: 4.419 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.37 2.73 4.8297 1 1 1 8 30.22 36.35 2.9576 2 2 0 12 35.59 100.00 2.5223 3 1 1 24 37.23 2.59 2.4149 2 2 2 8 43.26 18.92 2.0913 4 0 0 6 53.68 11.55 1.7076 4 2 2 24 57.22 25.97 1.6099 5 1 1 24 57.22 5.72 1.6099 3 3 3 8 62.84 43.50 1.4788 4 4 0 12 71.30 3.97 1.3227 6 2 0 24 74.36 8.29 1.2757 5 3 3 24 75.37 2.04 1.2611 6 2 2 24 79.36 2.33 1.2074 4 4 4 8 87.20 4.29 1.1179 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.