Duftite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from the powder pattern from R040160 Kharisun, Taylor M R, Bevan D J M, Pring A Mineralogical Magazine 62 (1998) 121-130 The crystal chemistry of duftite, PbCuAsO4(OH) and the beta-duftite problem Note: sample is synthetic CELL PARAMETERS: 7.401261 9.434908 5.923351 90.00000 90.00000 90.00000 SPACE GROUP: P2_12_12_1 X-RAY WAVELENGTH: 1.541838 2-THETA INTENSITY D-SPACING H K L 8.12 26.30 5.0166 0 1 1 8.63 12.40 4.7175 0 2 0 9.81 38.50 4.1526 1 1 1 10.24 14.32 3.9781 1 2 0 11.01 5.32 3.7006 2 0 0 11.04 1.28 3.6902 0 2 1 11.82 11.68 3.4451 2 1 0 12.34 12.04 3.3024 1 2 1 12.98 100.00 3.1385 2 0 1 13.69 1.10 2.9780 2 1 1 13.76 24.68 2.9617 0 0 2 14.00 3.70 2.9117 2 2 0 14.08 55.19 2.8945 1 3 0 15.45 41.39 2.6399 1 1 2 15.61 37.09 2.6130 2 2 1 15.68 50.50 2.6006 1 3 1 16.26 18.69 2.5083 0 2 2 17.10 9.38 2.3868 3 1 0 17.03 4.51 2.3965 2 3 0 17.18 3.82 2.3756 1 2 2 17.65 2.97 2.3123 2 0 2 18.44 4.13 2.2139 3 1 1 18.18 19.34 2.2459 2 1 2 18.68 5.37 2.1862 3 2 0 18.17 5.39 2.2474 1 4 0 19.92 8.08 2.0509 3 2 1 19.68 5.36 2.0763 2 2 2 19.44 5.21 2.1012 1 4 1 19.74 13.49 2.0701 1 3 2 20.55 1.64 1.9890 2 4 0 21.06 3.86 1.9411 3 3 0 21.16 2.36 1.9326 0 1 3 22.11 8.40 1.8503 4 0 0 21.87 5.76 1.8699 1 1 3 21.69 3.26 1.8856 2 4 1 22.18 19.06 1.8446 3 3 1 21.96 1.10 1.8630 2 3 2 22.46 1.51 1.8214 0 2 3 22.17 7.42 1.8451 0 4 2 23.58 5.69 1.7360 4 1 1 23.27 2.85 1.7589 3 2 2 23.77 12.87 1.7226 4 2 0 23.14 1.83 1.7686 1 2 3 22.86 2.29 1.7903 1 4 2 23.50 14.30 1.7420 2 0 3 22.76 5.11 1.7980 0 5 1 23.43 5.59 1.7471 1 5 1 24.37 3.48 1.6811 2 5 0 25.08 6.84 1.6342 2 2 3 25.01 2.10 1.6384 3 4 1 24.81 2.39 1.6512 2 4 2 25.24 23.27 1.6235 3 3 2 25.12 11.15 1.6311 1 3 3 26.13 15.86 1.5692 4 0 2 26.64 1.04 1.5399 4 3 1 26.97 1.78 1.5214 3 1 3 26.36 11.04 1.5559 1 5 2 26.92 1.22 1.5239 2 3 3 27.56 1.13 1.4890 4 2 2 26.08 4.96 1.5725 0 6 0 28.08 3.08 1.4624 5 1 0 27.38 4.23 1.4988 3 5 0 27.72 8.12 1.4808 0 0 4 28.02 1.89 1.4653 3 2 3 28.21 2.21 1.4558 4 4 0 28.94 1.67 1.4197 5 1 1 27.67 1.26 1.4833 1 4 3 28.26 4.55 1.4530 3 5 1 28.09 3.74 1.4620 2 5 2 28.62 1.04 1.4352 1 1 4 29.33 1.13 1.4013 2 4 3 29.70 6.52 1.3842 3 3 3 29.62 1.08 1.3878 1 2 4 29.23 10.69 1.4059 2 6 1 30.72 1.22 1.3393 5 3 0 30.78 1.88 1.3365 4 1 3 29.60 1.64 1.3889 0 6 2 30.14 1.63 1.3642 0 5 3 31.51 5.74 1.3063 5 3 1 30.76 1.23 1.3373 3 5 2 31.18 1.78 1.3199 2 2 4 30.66 2.24 1.3416 1 5 3 31.22 7.77 1.3183 1 3 4 31.94 2.89 1.2895 4 5 1 31.32 1.11 1.3142 0 7 1 32.75 2.61 1.2583 3 1 4 34.16 5.96 1.2076 6 0 1 33.80 8.74 1.2203 5 3 2 33.34 1.05 1.2365 1 4 4 35.30 2.21 1.1699 6 2 1 35.14 1.00 1.1751 5 1 3 34.44 1.79 1.1982 4 6 0 34.57 2.40 1.1938 3 5 3 34.75 1.63 1.1878 2 4 4 35.07 1.06 1.1773 3 3 4 35.46 1.44 1.1647 5 5 0 35.73 2.24 1.1562 4 0 4 36.57 1.23 1.1305 6 1 2 35.58 1.33 1.1609 1 1 5 36.17 1.24 1.1428 5 5 1 35.38 4.95 1.1673 2 6 3 35.47 1.19 1.1645 2 7 2 36.83 4.27 1.1229 4 2 4 36.65 2.72 1.1283 2 0 5 37.33 2.85 1.1084 5 3 3 36.17 1.68 1.1428 1 8 1 37.25 7.15 1.1108 4 6 2 37.23 1.28 1.1112 2 5 4 37.72 1.60 1.0973 2 2 5 37.69 1.46 1.0980 4 5 3 37.75 2.04 1.0964 1 3 5 37.75 2.04 1.0964 1 3 5 XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.