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: SA1-51 _database_code_amcsd 0007154 CELL PARAMETERS: 5.3360 9.2360 10.2230 90.000 100.058 90.000 SPACE GROUP: C2/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 496.080 Density (g/cm3): 2.982 MAX. ABS. INTENSITY / VOLUME**2: 12.11491809 RIR: 1.323 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 8.78 100.00 10.0659 0 0 1 2 19.22 6.16 4.6180 0 2 0 2 19.44 8.02 4.5668 1 1 0 4 20.09 1.81 4.4188 -1 1 1 4 22.57 10.45 3.9398 1 1 1 4 24.25 26.35 3.6707 -1 1 2 4 26.19 35.55 3.4027 0 2 2 4 26.57 36.91 3.3553 0 0 3 2 28.31 33.41 3.1523 1 1 2 4 30.57 22.57 2.9240 -1 1 3 4 33.00 11.39 2.7145 0 2 3 4 33.72 2.36 2.6578 -2 0 1 2 33.74 4.81 2.6562 1 3 0 4 34.13 25.14 2.6270 2 0 0 2 34.14 50.12 2.6262 -1 3 1 4 35.52 4.28 2.5271 1 1 3 4 35.68 5.95 2.5165 0 0 4 2 35.71 1.22 2.5141 1 3 1 4 36.84 12.63 2.4399 2 0 1 2 36.84 24.95 2.4397 -1 3 2 4 39.01 1.75 2.3090 0 4 0 2 39.10 3.33 2.3035 -2 2 1 4 39.46 3.92 2.2834 2 2 0 4 39.71 3.19 2.2698 -2 0 3 2 39.74 6.36 2.2679 1 3 2 4 40.06 3.86 2.2505 0 4 1 4 40.84 3.59 2.2094 -2 2 2 4 41.45 23.50 2.1783 -1 3 3 4 41.46 11.72 2.1780 2 0 2 2 41.88 2.57 2.1573 2 2 1 4 43.10 1.43 2.0987 0 4 2 4 45.03 5.91 2.0132 0 0 5 2 45.34 5.97 2.0001 -2 0 4 2 45.38 11.79 1.9985 1 3 3 4 47.53 4.28 1.9131 -1 3 4 4 47.54 2.11 1.9126 2 0 3 2 53.91 2.05 1.7006 1 5 1 4 54.71 1.26 1.6776 0 0 6 2 54.72 17.73 1.6773 -1 3 5 4 54.73 3.31 1.6771 2 4 1 4 54.74 8.96 1.6768 2 0 4 2 55.69 4.08 1.6504 -3 1 3 4 55.72 1.51 1.6497 3 1 1 4 56.88 2.17 1.6187 -2 4 3 4 56.91 3.47 1.6180 1 5 2 4 58.23 1.95 1.5845 -1 5 3 4 58.23 2.40 1.5844 2 4 2 4 59.67 1.13 1.5497 -3 1 4 4 59.70 1.25 1.5488 3 1 2 4 60.02 5.33 1.5413 -2 0 6 2 60.07 10.64 1.5403 1 3 5 4 60.07 21.60 1.5401 -3 3 1 4 60.11 10.76 1.5393 0 6 0 2 60.84 2.72 1.5225 -3 3 2 4 60.85 2.68 1.5223 3 3 0 4 60.88 2.70 1.5216 0 6 1 4 62.85 2.28 1.4786 -1 3 6 4 62.87 1.11 1.4781 2 0 5 2 64.84 1.49 1.4380 0 0 7 2 64.97 1.01 1.4354 -1 1 7 4 66.41 1.28 1.4078 2 2 5 4 68.73 5.11 1.3658 -2 0 7 2 68.77 10.13 1.3651 1 3 6 4 69.22 1.75 1.3572 0 4 6 4 70.72 1.83 1.3320 -2 6 1 4 70.92 3.05 1.3289 -4 0 2 2 70.97 6.15 1.3281 2 6 0 4 71.85 2.94 1.3140 -3 3 5 4 71.89 2.92 1.3133 3 3 3 4 71.90 2.95 1.3131 0 6 4 4 72.12 2.03 1.3098 -2 2 7 4 72.56 2.10 1.3028 -4 0 3 2 72.62 4.17 1.3019 2 6 1 4 74.46 1.25 1.2742 4 0 1 2 74.48 2.49 1.2740 -2 6 3 4 75.20 1.82 1.2635 2 2 6 4 75.57 1.37 1.2582 0 0 8 2 75.94 1.42 1.2530 -1 7 2 4 76.75 1.83 1.2418 -3 5 3 4 77.75 1.49 1.2283 4 2 1 4 78.33 1.09 1.2206 0 4 7 4 80.01 1.01 1.1992 2 6 3 4 85.58 2.47 1.1349 -4 0 6 2 85.66 4.91 1.1340 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.