Pyromorphite Okudera H American Mineralogist 98 (2013) 1573-1579 Relationships among channel typology and atomic displacements in the structures of Pb5(BO4)3Cl with B = P (pyromorphite), V (vanadinite), and As (mimetite) Locality: Daoping mine, Guangxi, China _database_code_amcsd 0020246 CELL PARAMETERS: 9.9860 9.9860 7.3378 90.000 90.000 120.000 SPACE GROUP: P6_3/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 633.694 Density (g/cm3): 6.756 MAX. ABS. INTENSITY / VOLUME**2: 145.9737031 RIR: 7.035 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 17.76 9.13 4.9930 1 1 0 6 20.54 28.05 4.3241 2 0 0 6 21.53 43.91 4.1280 1 1 1 12 23.89 2.12 3.7253 2 0 1 12 24.26 6.86 3.6689 0 0 2 2 26.39 29.61 3.3775 1 0 2 12 27.28 15.71 3.2687 1 2 0 6 27.28 19.43 3.2687 2 1 0 6 29.93 41.90 2.9858 1 2 1 12 29.93 50.90 2.9858 2 1 1 12 30.23 100.00 2.9565 1 1 2 12 31.02 53.72 2.8827 3 0 0 6 35.97 2.66 2.4965 2 2 0 6 36.83 1.35 2.4406 1 2 2 12 39.77 5.75 2.2667 3 0 2 12 41.09 15.00 2.1965 1 1 3 12 41.78 5.90 2.1620 4 0 0 6 43.86 36.26 2.0640 2 2 2 12 45.16 7.76 2.0076 1 3 2 12 45.16 11.96 2.0076 3 1 2 12 45.73 6.98 1.9840 2 3 0 6 45.73 2.42 1.9840 3 2 0 6 46.36 14.81 1.9584 1 2 3 12 46.36 11.70 1.9584 2 1 3 12 47.47 13.58 1.9152 2 3 1 12 47.47 9.30 1.9152 3 2 1 12 48.22 9.16 1.8872 1 4 0 6 48.22 14.42 1.8872 4 1 0 6 48.90 30.03 1.8627 4 0 2 12 49.70 12.40 1.8345 0 0 4 2 53.19 1.82 1.7219 1 1 4 12 54.32 3.43 1.6888 2 0 4 12 54.69 2.81 1.6782 1 4 2 12 54.69 1.54 1.6782 4 1 2 12 55.19 1.08 1.6643 3 3 0 6 56.29 3.37 1.6343 2 4 0 6 56.29 2.05 1.6343 4 2 0 6 56.71 5.37 1.6231 3 3 1 12 57.62 5.68 1.5997 1 2 4 12 57.62 3.56 1.5997 2 1 4 12 59.04 5.00 1.5645 5 0 2 12 59.51 1.49 1.5532 1 5 0 6 59.51 2.40 1.5532 5 1 0 6 59.75 12.27 1.5477 3 0 4 12 60.04 3.28 1.5408 2 3 3 12 60.04 5.33 1.5408 3 2 3 12 60.97 3.93 1.5196 1 5 1 12 60.97 5.89 1.5196 5 1 1 12 61.15 9.84 1.5157 3 3 2 12 66.40 1.88 1.4080 1 1 5 12 66.89 2.98 1.3988 4 0 4 12 68.15 2.38 1.3760 3 3 3 12 69.02 1.68 1.3608 2 5 1 12 69.02 3.24 1.3608 5 2 1 12 69.83 2.67 1.3469 2 3 4 12 69.83 1.09 1.3469 3 2 4 12 70.15 6.54 1.3415 6 0 2 12 70.31 2.39 1.3388 1 2 5 12 70.31 4.11 1.3388 2 1 5 12 71.12 4.20 1.3257 3 4 2 12 71.12 1.32 1.3257 4 3 2 12 71.54 1.34 1.3188 1 6 0 6 71.54 1.03 1.3188 6 1 0 6 71.76 5.51 1.3154 1 4 4 12 71.76 6.84 1.3154 4 1 4 12 72.02 2.55 1.3112 1 5 3 12 72.02 2.56 1.3112 5 1 3 12 72.87 2.30 1.2980 1 6 1 12 72.87 1.39 1.2980 6 1 1 12 73.03 5.93 1.2956 2 5 2 12 73.03 5.17 1.2956 5 2 2 12 76.28 2.05 1.2483 4 4 0 6 78.36 2.19 1.2203 2 4 4 12 78.36 2.23 1.2203 4 2 4 12 79.08 1.20 1.2109 1 0 6 12 79.54 1.05 1.2051 2 5 3 12 79.54 2.34 1.2051 5 2 3 12 80.93 5.14 1.1879 1 1 6 12 81.13 1.98 1.1854 5 1 4 12 81.13 1.38 1.1854 1 5 4 12 81.60 1.17 1.1799 3 2 5 12 81.60 2.66 1.1799 2 3 5 12 82.36 1.74 1.1708 7 0 2 12 83.23 1.17 1.1608 1 6 3 12 88.91 1.27 1.1008 3 3 5 12 89.17 3.54 1.0983 2 2 6 12 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.