Magnesioferrite Boiocchi M, Caucia F, Merli M, Prella D, Ungaretti L European Journal of Mineralogy 13 (2001) 871-881 Crystal-chemical reasons for the immiscibility of periclase and wustite under lithospheric P,T conditions Sample: after heating to 1100 deg C _database_code_amcsd 0006905 CELL PARAMETERS: 8.3850 8.3850 8.3850 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 589.534 Density (g/cm3): 4.477 MAX. ABS. INTENSITY / VOLUME**2: 59.49970179 RIR: 4.327 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.33 8.12 4.8411 1 1 1 8 30.15 30.47 2.9645 2 2 0 12 35.51 100.00 2.5282 3 1 1 24 37.14 3.71 2.4205 2 2 2 8 43.16 24.35 2.0963 4 0 0 6 53.54 10.18 1.7116 4 2 2 24 57.08 27.52 1.6137 5 1 1 24 57.08 5.78 1.6137 3 3 3 8 62.68 47.16 1.4823 4 4 0 12 71.11 3.68 1.3258 6 2 0 24 74.15 8.90 1.2787 5 3 3 24 75.16 2.57 1.2641 6 2 2 24 79.13 3.12 1.2103 4 4 4 8 86.95 4.25 1.1205 6 4 2 48 89.85 5.98 1.0916 5 5 3 24 89.85 8.14 1.0916 7 3 1 48 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.