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: N7g, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite _database_code_amcsd 0003626 CELL PARAMETERS: 8.3091 8.3091 8.3091 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 573.670 Density (g/cm3): 4.469 MAX. ABS. INTENSITY / VOLUME**2: 49.74413150 RIR: 3.624 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.50 37.34 4.7973 1 1 1 8 30.43 22.09 2.9377 2 2 0 12 35.84 100.00 2.5053 3 1 1 24 37.50 6.86 2.3986 2 2 2 8 43.57 38.79 2.0773 4 0 0 6 47.71 1.09 1.9062 3 3 1 24 54.07 6.50 1.6961 4 2 2 24 57.65 4.32 1.5991 3 3 3 8 57.65 33.37 1.5991 5 1 1 24 63.32 50.52 1.4689 4 4 0 12 66.58 4.12 1.4045 5 3 1 48 71.86 2.10 1.3138 6 2 0 24 74.95 9.10 1.2671 5 3 3 24 75.97 4.55 1.2526 6 2 2 24 80.00 4.95 1.1993 4 4 4 8 82.99 2.19 1.1635 5 5 1 24 87.94 3.25 1.1104 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.