Magnesiochromite Bosi F, Andreozzi G B, Ferrini V, Lucchesi S American Mineralogist 89 (2004) 1367-1373 Behavior of cation vacany in kenotetrahedral Cr-spinels from Albanian eastern belt ophiolites Sample: Shkm3g, Provenance is Shkalla, Bulqiza massif, Sequence is tectonite _database_code_amcsd 0003634 CELL PARAMETERS: 8.2982 8.2982 8.2982 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 571.415 Density (g/cm3): 4.340 MAX. ABS. INTENSITY / VOLUME**2: 45.00278350 RIR: 3.376 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.52 37.06 4.7910 1 1 1 8 30.47 22.82 2.9339 2 2 0 12 35.89 100.00 2.5020 3 1 1 24 37.55 5.45 2.3955 2 2 2 8 43.63 40.08 2.0745 4 0 0 6 54.15 6.68 1.6939 4 2 2 24 57.73 33.99 1.5970 5 1 1 24 57.73 4.19 1.5970 3 3 3 8 63.41 51.87 1.4669 4 4 0 12 66.68 4.00 1.4027 5 3 1 48 71.97 2.15 1.3121 6 2 0 24 75.06 9.11 1.2655 5 3 3 24 76.08 4.07 1.2510 6 2 2 24 80.13 5.04 1.1977 4 4 4 8 83.13 2.22 1.1620 5 5 1 24 88.09 3.37 1.1089 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.