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: N10a, Provenance is Bulqize, Bulqiza massif, Sequence is tectonite _database_code_amcsd 0003625 CELL PARAMETERS: 8.3133 8.3133 8.3133 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 574.540 Density (g/cm3): 4.415 MAX. ABS. INTENSITY / VOLUME**2: 48.41260229 RIR: 3.571 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.49 31.90 4.7997 1 1 1 8 30.41 24.28 2.9392 2 2 0 12 35.82 100.00 2.5066 3 1 1 24 37.48 5.61 2.3998 2 2 2 8 43.55 36.48 2.0783 4 0 0 6 54.04 7.16 1.6969 4 2 2 24 57.61 4.26 1.5999 3 3 3 8 57.61 33.34 1.5999 5 1 1 24 63.28 50.21 1.4696 4 4 0 12 66.54 3.40 1.4052 5 3 1 48 71.82 2.32 1.3144 6 2 0 24 74.90 9.01 1.2678 5 3 3 24 75.92 3.94 1.2533 6 2 2 24 79.95 4.55 1.1999 4 4 4 8 82.94 1.94 1.1641 5 5 1 24 87.89 3.52 1.1109 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.