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 = 1045 K, P = 3 GPa during heating _database_code_amcsd 0003911 CELL PARAMETERS: 8.4012 8.4012 8.4012 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 592.964 Density (g/cm3): 4.480 MAX. ABS. INTENSITY / VOLUME**2: 60.32271325 RIR: 4.384 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.29 3.44 4.8505 1 1 1 8 30.09 34.97 2.9703 2 2 0 12 35.44 100.00 2.5331 3 1 1 24 37.07 2.82 2.4252 2 2 2 8 43.07 19.69 2.1003 4 0 0 6 53.43 11.25 1.7149 4 2 2 24 56.95 25.59 1.6168 5 1 1 24 56.95 5.80 1.6168 3 3 3 8 62.54 43.36 1.4851 4 4 0 12 70.95 3.91 1.3284 6 2 0 24 73.99 8.23 1.2812 5 3 3 24 74.99 2.08 1.2665 6 2 2 24 78.95 2.33 1.2126 4 4 4 8 86.74 4.19 1.1227 6 4 2 48 89.63 7.52 1.0937 7 3 1 48 89.63 5.17 1.0937 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.