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-TF6 Locality:Middle Atlas Neogene-Quaternary Volcanic Field of Morocco _database_code_amcsd 0020065 CELL PARAMETERS: 8.1339 8.1339 8.1339 90.000 90.000 90.000 SPACE GROUP: Fd3m X-RAY WAVELENGTH: 1.541838 Cell Volume: 538.141 Density (g/cm3): 3.872 MAX. ABS. INTENSITY / VOLUME**2: 27.46400442 RIR: 2.309 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 18.90 18.82 4.6961 1 1 1 8 31.10 37.06 2.8758 2 2 0 12 36.64 100.00 2.4525 3 1 1 24 44.56 38.06 2.0335 4 0 0 6 55.33 10.56 1.6603 4 2 2 24 59.01 3.56 1.5654 3 3 3 8 59.01 39.28 1.5654 5 1 1 24 64.84 60.05 1.4379 4 4 0 12 68.21 1.79 1.3749 5 3 1 48 73.66 3.35 1.2861 6 2 0 24 76.85 9.75 1.2404 5 3 3 24 77.91 1.50 1.2262 6 2 2 24 82.09 4.51 1.1740 4 4 4 8 85.20 1.77 1.1390 5 5 1 24 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.