Spinel Lenaz D, Youbi N, Min A D, Boumehdi M A, Abbou M B American Mineralogist 99 (2014) 267-275 Low intra-crystalline closure temperatures of Cr-bearing spinels from the mantle xenoliths of the Middle AtlasNeogene-Quaternary Volcanic Field (Morocco):Mineralogical evidence of a cooler mantle beneath the West African Craton. Note:Sample MAR-BI24 Locality:Middle Atlas Neogene-Quaternary Volcanic Field of Morocco _database_code_amcsd 0020064 CELL PARAMETERS: 8.1727 8.1727 8.1727 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 545.879 Density (g/cm3): 4.074 MAX. ABS. INTENSITY / VOLUME**2: 33.57311324 RIR: 2.683 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.81 21.16 4.7185 1 1 1 8 30.95 33.42 2.8895 2 2 0 12 36.46 100.00 2.4642 3 1 1 24 44.33 35.95 2.0432 4 0 0 6 55.05 9.45 1.6682 4 2 2 24 58.70 3.75 1.5728 3 3 3 8 58.70 36.73 1.5728 5 1 1 24 64.50 55.33 1.4447 4 4 0 12 67.84 2.12 1.3814 5 3 1 48 73.25 2.96 1.2922 6 2 0 24 76.42 9.29 1.2463 5 3 3 24 77.47 2.13 1.2321 6 2 2 24 81.62 4.33 1.1796 4 4 4 8 84.70 1.76 1.1444 5 5 1 24 89.80 4.66 1.0921 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.