Phlogopite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from the powder pattern for R070330 Russell R L, Guggenheim S The Canadian Mineralogist 37 (1999) 711-720 The crystal structures of near-end-member phlogopite at high temperatures and heat-treated Fe-rich phlogopite: The influence of the O, OH, F site Sample: T = 20 deg C Locality: White Well, Australia CELL PARAMETERS: 5.372501 9.162053 10.29665 90.00000 100.4994 90.00000 SPACE GROUP: C2/m X-RAY WAVELENGTH: 1.541838 2-THETA INTENSITY D-SPACING H K L 8.74 100.00 10.1242 0 0 1 17.51 5.62 5.0621 0 0 2 19.37 14.58 4.5810 0 2 0 19.39 19.14 4.5764 1 1 0 19.98 4.98 4.4416 -1 1 1 22.54 12.16 3.9430 1 1 1 24.06 30.51 3.6975 -1 1 2 26.22 39.88 3.3967 0 2 2 26.40 45.61 3.3747 0 0 3 28.26 36.09 3.1559 1 1 2 30.31 23.84 2.9474 -1 1 3 32.95 10.90 2.7171 0 2 3 33.45 3.63 2.6777 -2 0 1 33.89 7.28 2.6440 1 3 0 34.24 47.48 2.6172 -1 3 1 33.92 24.01 2.6413 2 0 0 35.43 3.00 2.5319 1 1 3 35.45 4.50 2.5311 0 0 4 35.33 5.06 2.5391 -2 0 2 35.86 9.90 2.5030 1 3 1 36.87 29.02 2.4365 -1 3 2 36.67 14.35 2.4490 2 0 1 39.31 1.30 2.2905 0 4 0 38.94 2.30 2.3117 -2 2 1 39.35 2.55 2.2882 2 2 0 39.28 3.90 2.2926 -2 0 3 39.86 7.69 2.2605 1 3 2 40.35 2.54 2.2341 0 4 1 40.60 2.82 2.2208 -2 2 2 41.39 21.73 2.1800 -1 3 3 41.31 10.79 2.1841 2 0 2 41.80 2.10 2.1598 2 2 1 43.33 1.11 2.0868 0 4 2 44.73 9.31 2.0248 0 0 5 44.83 5.32 2.0206 -2 0 4 45.44 10.52 1.9948 1 3 3 47.37 5.91 1.9178 -1 3 4 47.39 3.00 1.9173 2 0 3 49.26 1.79 1.8488 -2 2 4 51.65 1.74 1.7686 2 2 3 52.23 1.92 1.7503 1 3 4 52.00 1.75 1.7575 -3 1 1 52.54 2.06 1.7406 -2 4 1 53.10 1.46 1.7236 -1 5 1 53.95 1.38 1.6983 0 4 4 54.25 1.70 1.6898 1 5 1 54.47 16.27 1.6834 -1 3 5 54.56 8.07 1.6808 2 0 4 54.84 3.18 1.6729 2 4 1 55.14 4.31 1.6646 -3 1 3 56.78 1.37 1.6204 -2 4 3 57.22 3.57 1.6089 1 5 2 58.40 1.07 1.5791 -1 5 3 58.34 2.12 1.5807 2 4 2 59.34 4.44 1.5565 -2 0 6 59.98 8.84 1.5412 1 3 5 59.83 24.00 1.5448 -3 3 1 60.60 11.95 1.5270 0 6 0 60.52 3.78 1.5288 -3 3 2 60.67 3.74 1.5255 3 3 0 61.36 3.76 1.5099 0 6 1 62.49 4.19 1.4851 -1 3 6 62.65 2.07 1.4819 2 0 5 64.37 2.19 1.4463 0 0 7 66.24 1.33 1.4099 2 2 5 66.32 1.62 1.4085 -3 3 4 67.25 1.61 1.3912 0 6 3 66.73 1.64 1.4008 3 3 2 67.93 8.10 1.3788 -2 0 7 68.61 16.12 1.3670 1 3 6 69.09 1.95 1.3585 0 4 6 70.11 1.00 1.3413 -4 0 1 71.01 2.02 1.3265 -2 6 1 70.26 2.73 1.3388 -4 0 2 71.29 5.45 1.3220 2 6 0 71.39 2.14 1.3203 -2 2 7 71.23 2.41 1.3229 -3 3 5 72.20 2.39 1.3075 0 6 4 71.77 2.38 1.3143 3 3 3 71.80 3.00 1.3137 -4 0 3 72.96 6.00 1.2958 2 6 1 73.96 1.09 1.2807 -3 5 1 74.66 1.20 1.2704 1 7 0 74.62 3.57 1.2709 -2 6 3 74.01 1.79 1.2800 4 0 1 74.97 1.47 1.2659 2 2 6 75.00 1.23 1.2655 0 0 8 76.44 1.34 1.2452 -1 7 2 76.57 1.75 1.2434 -3 5 3 77.35 1.52 1.2328 4 2 1 80.32 1.31 1.1945 2 6 3 84.45 2.44 1.1463 -4 0 6 85.94 4.90 1.1302 2 6 4 85.94 4.90 1.1302 2 6 4 XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.