Phlogopite Scordari F, Ventruti G, Sabato A, Bellatreccia F, Della Ventura G, Pedrazzi G European Journal of Mineralogy 18 (2006) 379-391 Ti-rich phlogopite from Mt. Vulture (Potenza, Italy) investigated by a multianalytical, approach: substitutional mechanisms and orientation of the OH dipoles Locality: Cava St. Antonio, Mt. Vulture, Potenza, Italy Sample: SA1-9 _database_code_amcsd 0007153 CELL PARAMETERS: 5.3370 9.2380 10.2280 90.000 100.050 90.000 SPACE GROUP: C2/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 496.536 Density (g/cm3): 2.968 MAX. ABS. INTENSITY / VOLUME**2: 12.32542813 RIR: 1.352 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 8.78 100.00 10.0711 0 0 1 2 19.22 6.41 4.6190 0 2 0 2 19.43 8.24 4.5678 1 1 0 4 20.09 2.01 4.4197 -1 1 1 4 22.56 9.71 3.9411 1 1 1 4 24.24 25.46 3.6717 -1 1 2 4 26.18 33.98 3.4039 0 2 2 4 26.55 36.60 3.3570 0 0 3 2 28.30 32.39 3.1535 1 1 2 4 30.56 21.38 2.9250 -1 1 3 4 32.98 10.92 2.7156 0 2 3 4 33.72 2.27 2.6583 -2 0 1 2 33.74 4.63 2.6568 1 3 0 4 34.12 24.30 2.6276 2 0 0 2 34.13 48.31 2.6267 -1 3 1 4 35.51 3.97 2.5282 1 1 3 4 35.66 5.82 2.5178 0 0 4 2 35.70 1.31 2.5148 1 3 1 4 36.83 12.50 2.4405 2 0 1 2 36.83 24.72 2.4403 -1 3 2 4 39.00 1.62 2.3095 0 4 0 2 39.10 3.25 2.3040 -2 2 1 4 39.46 3.67 2.2839 2 2 0 4 39.70 3.18 2.2703 -2 0 3 2 39.73 6.30 2.2686 1 3 2 4 40.05 3.78 2.2511 0 4 1 4 40.83 3.41 2.2099 -2 2 2 4 41.44 22.62 2.1790 -1 3 3 4 41.44 11.30 2.1788 2 0 2 2 41.86 2.42 2.1578 2 2 1 4 43.09 1.26 2.0992 0 4 2 4 45.01 5.77 2.0142 0 0 5 2 45.33 5.77 2.0007 -2 0 4 2 45.36 11.39 1.9992 1 3 3 4 47.51 4.23 1.9137 -1 3 4 4 47.52 2.10 1.9134 2 0 3 2 53.90 1.97 1.7010 1 5 1 4 54.68 1.18 1.6785 0 0 6 2 54.70 17.21 1.6779 -1 3 5 4 54.72 8.68 1.6775 2 0 4 2 54.72 3.26 1.6775 2 4 1 4 55.68 3.87 1.6507 -3 1 3 4 55.70 1.44 1.6501 3 1 1 4 56.87 2.10 1.6190 -2 4 3 4 56.89 3.33 1.6184 1 5 2 4 58.21 1.88 1.5849 -1 5 3 4 58.21 2.27 1.5848 2 4 2 4 59.65 1.10 1.5500 -3 1 4 4 59.68 1.21 1.5493 3 1 2 4 60.00 5.10 1.5418 -2 0 6 2 60.04 10.19 1.5410 1 3 5 4 60.06 21.00 1.5404 -3 3 1 4 60.09 10.46 1.5397 0 6 0 2 60.83 2.72 1.5228 -3 3 2 4 60.84 2.67 1.5226 3 3 0 4 60.86 2.69 1.5220 0 6 1 4 62.82 2.32 1.4792 -1 3 6 4 62.84 1.13 1.4788 2 0 5 2 64.80 1.46 1.4387 0 0 7 2 66.37 1.24 1.4084 2 2 5 4 68.69 5.08 1.3664 -2 0 7 2 68.73 10.04 1.3657 1 3 6 4 69.19 1.68 1.3578 0 4 6 4 70.71 1.79 1.3323 -2 6 1 4 70.90 2.96 1.3291 -4 0 2 2 70.95 5.97 1.3284 2 6 0 4 71.83 2.85 1.3143 -3 3 5 4 71.86 2.82 1.3137 3 3 3 4 71.88 2.85 1.3135 0 6 4 4 72.08 1.97 1.3102 -2 2 7 4 72.55 2.08 1.3030 -4 0 3 2 72.60 4.14 1.3022 2 6 1 4 74.44 1.25 1.2745 4 0 1 2 74.46 2.47 1.2743 -2 6 3 4 75.16 1.76 1.2641 2 2 6 4 75.52 1.31 1.2589 0 0 8 2 75.92 1.40 1.2533 -1 7 2 4 76.73 1.77 1.2420 -3 5 3 4 77.73 1.45 1.2286 4 2 1 4 78.29 1.06 1.2212 0 4 7 4 79.98 1.00 1.1995 2 6 3 4 85.55 2.41 1.1352 -4 0 6 2 85.63 4.79 1.1343 2 6 4 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.