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: N2h, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite _database_code_amcsd 0003632 CELL PARAMETERS: 8.3071 8.3071 8.3071 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 573.256 Density (g/cm3): 4.403 MAX. ABS. INTENSITY / VOLUME**2: 47.52273966 RIR: 3.514 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.50 34.91 4.7961 1 1 1 8 30.44 23.09 2.9370 2 2 0 12 35.85 100.00 2.5047 3 1 1 24 37.50 5.88 2.3981 2 2 2 8 43.58 38.33 2.0768 4 0 0 6 54.08 6.80 1.6957 4 2 2 24 57.66 4.27 1.5987 3 3 3 8 57.66 33.34 1.5987 5 1 1 24 63.33 50.72 1.4685 4 4 0 12 66.60 3.76 1.4042 5 3 1 48 71.88 2.20 1.3135 6 2 0 24 74.97 9.02 1.2668 5 3 3 24 75.99 4.11 1.2523 6 2 2 24 80.02 4.81 1.1990 4 4 4 8 83.02 2.07 1.1632 5 5 1 24 87.97 3.36 1.1101 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.