Mottramite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from the powder pattern for R050521 Cooper M A, Hawthorne F C The Canadian Mineralogist 33 (1995) 1119-1124 The crystal structure of mottramite, and the nature of Cu=Zn solid solution in the mottramite-descloizite series CELL PARAMETERS: 7.691245 6.045510 9.227469 90.00000 90.00000 90.00000 SPACE GROUP: Pnma X-RAY WAVELENGTH: 1.541838 2-THETA INTENSITY D-SPACING H K L 17.55 63.91 5.0569 0 1 1 19.25 13.63 4.6137 0 0 2 21.03 36.24 4.2254 1 1 1 22.48 22.63 3.9565 1 0 2 23.13 3.52 3.8456 2 0 0 25.09 25.43 3.5497 2 0 1 26.93 16.49 3.3105 1 1 2 27.49 100.00 3.2448 2 1 0 29.55 26.97 3.0228 0 2 0 30.25 6.12 2.9540 2 0 2 31.32 56.66 2.8559 1 0 3 33.29 42.91 2.6910 1 2 1 33.77 42.54 2.6541 2 1 2 34.73 56.82 2.5823 1 1 3 35.50 22.01 2.5284 0 2 2 36.36 9.92 2.4702 3 0 1 37.43 1.89 2.4020 2 0 3 37.43 6.74 2.4020 1 2 2 37.85 5.64 2.3765 2 2 0 39.13 37.06 2.3014 2 2 1 39.39 2.05 2.2867 3 1 1 40.23 5.92 2.2410 3 0 2 40.83 11.31 2.2096 1 0 4 42.79 3.28 2.1127 2 2 2 43.03 12.30 2.1013 3 1 2 43.60 10.95 2.0753 1 1 4 43.59 12.35 2.0759 1 2 3 45.86 2.04 1.9782 2 0 4 46.07 4.53 1.9693 3 0 3 46.09 5.86 1.9688 0 3 1 47.26 7.35 1.9228 4 0 0 47.66 3.89 1.9073 1 3 1 48.39 1.63 1.8801 2 1 4 48.60 14.50 1.8725 3 1 3 49.70 6.68 1.8338 0 2 4 50.69 3.11 1.8002 3 2 2 50.83 2.79 1.7957 1 3 2 51.19 6.13 1.7838 1 2 4 50.78 10.05 1.7973 4 1 1 51.15 15.08 1.7849 2 3 0 51.77 4.97 1.7651 0 1 5 51.47 13.72 1.7748 4 0 2 53.22 7.62 1.7204 1 1 5 53.41 1.86 1.7148 3 0 4 55.18 2.99 1.6638 2 0 5 55.15 8.49 1.6647 2 3 2 55.49 1.53 1.6553 2 2 4 55.69 5.14 1.6498 3 1 4 55.68 27.67 1.6501 3 2 3 55.81 12.61 1.6465 1 3 3 56.71 15.02 1.6224 4 2 0 59.91 12.88 1.5431 1 2 5 60.14 4.85 1.5379 0 0 6 61.31 9.73 1.5114 0 4 0 61.04 2.30 1.5173 5 0 1 61.92 5.83 1.4978 3 0 5 61.89 3.52 1.4984 3 3 2 62.33 3.00 1.4889 1 3 4 62.89 1.56 1.4770 4 0 4 63.15 1.82 1.4717 5 1 1 63.83 3.25 1.4576 2 2 5 64.01 4.34 1.4538 3 1 5 63.74 1.36 1.4593 5 0 2 66.15 1.90 1.4119 1 4 2 66.33 5.02 1.4085 3 3 3 67.34 9.95 1.3897 2 1 6 67.30 3.01 1.3906 2 4 1 68.41 1.33 1.3707 0 2 6 68.13 3.86 1.3756 4 3 1 68.96 1.78 1.3610 0 3 5 70.08 1.87 1.3421 3 2 5 70.19 2.95 1.3402 1 3 5 70.11 6.59 1.3415 5 1 3 70.45 8.01 1.3358 1 4 3 71.79 1.46 1.3142 5 2 2 72.31 2.03 1.3060 3 3 4 72.68 2.27 1.3003 4 1 5 73.49 2.29 1.2879 0 1 7 73.40 2.12 1.2892 3 4 1 74.03 1.77 1.2798 5 0 4 76.32 1.44 1.2470 2 0 7 75.89 1.23 1.2530 3 4 2 76.29 2.40 1.2475 1 4 4 75.95 6.00 1.2522 5 2 3 75.82 4.70 1.2540 6 1 0 79.09 1.86 1.2101 6 1 2 79.72 2.01 1.2021 3 3 5 79.81 1.30 1.2010 4 0 6 79.97 1.48 1.1990 3 4 3 80.84 2.19 1.1882 4 4 0 81.39 1.06 1.1816 5 0 5 81.65 1.98 1.1785 5 2 4 82.80 4.80 1.1651 2 3 6 82.32 2.00 1.1706 6 2 1 83.27 1.85 1.1597 5 1 5 83.88 2.67 1.1527 2 2 7 83.82 2.89 1.1534 2 5 0 84.07 4.58 1.1507 4 4 2 85.39 3.45 1.1362 5 3 3 87.05 1.32 1.1187 2 4 5 87.30 6.18 1.1161 4 2 6 87.03 1.91 1.1190 2 5 2 87.57 2.52 1.1134 1 5 3 87.82 1.25 1.1109 4 3 5 88.60 1.26 1.1032 0 3 7 90.29 3.17 1.0868 2 1 8 90.29 3.17 1.0868 2 1 8 XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.