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 0020247 CELL PARAMETERS: 9.9791 9.9791 7.3439 90.000 90.000 120.000 SPACE GROUP: P6_3/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 633.345 Density (g/cm3): 6.760 MAX. ABS. INTENSITY / VOLUME**2: 146.2664522 RIR: 7.045 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 17.78 9.20 4.9896 1 1 0 6 20.55 28.01 4.3211 2 0 0 6 21.53 43.71 4.1271 1 1 1 12 23.89 2.13 3.7242 2 0 1 12 24.24 6.88 3.6720 0 0 2 2 26.37 29.75 3.3795 1 0 2 12 27.30 15.60 3.2664 1 2 0 6 27.30 19.56 3.2664 2 1 0 6 29.94 41.98 2.9845 1 2 1 12 29.94 50.80 2.9845 2 1 1 12 30.22 100.00 2.9574 1 1 2 12 31.04 53.16 2.8807 3 0 0 6 36.00 2.72 2.4948 2 2 0 6 36.83 1.36 2.4405 1 2 2 12 39.77 5.73 2.2665 3 0 2 12 41.07 15.00 2.1977 1 1 3 12 41.81 5.85 2.1605 4 0 0 6 43.87 36.26 2.0636 2 2 2 12 45.17 11.86 2.0071 3 1 2 12 45.17 7.80 2.0071 1 3 2 12 45.76 6.89 1.9826 2 3 0 6 45.76 2.46 1.9826 3 2 0 6 46.35 14.80 1.9589 1 2 3 12 46.35 11.75 1.9589 2 1 3 12 47.50 13.49 1.9141 2 3 1 12 47.50 9.29 1.9141 3 2 1 12 48.26 9.12 1.8859 1 4 0 6 48.26 14.48 1.8859 4 1 0 6 48.91 30.00 1.8621 4 0 2 12 49.66 12.34 1.8360 0 0 4 2 53.16 1.84 1.7230 1 1 4 12 54.29 3.42 1.6898 2 0 4 12 54.72 2.78 1.6776 1 4 2 12 54.72 1.54 1.6776 4 1 2 12 55.23 1.06 1.6632 3 3 0 6 56.33 3.34 1.6332 2 4 0 6 56.33 2.05 1.6332 4 2 0 6 56.75 5.47 1.6221 3 3 1 12 57.59 5.74 1.6005 1 2 4 12 57.59 3.60 1.6005 2 1 4 12 59.07 5.09 1.5638 5 0 2 12 59.56 1.47 1.5522 1 5 0 6 59.56 2.34 1.5522 5 1 0 6 59.73 12.25 1.5483 3 0 4 12 60.05 5.27 1.5407 3 2 3 12 60.05 3.24 1.5407 2 3 3 12 61.01 3.94 1.5186 1 5 1 12 61.01 5.86 1.5186 5 1 1 12 61.17 9.81 1.5150 3 3 2 12 66.34 1.89 1.4090 1 1 5 12 66.88 2.99 1.3991 4 0 4 12 68.16 2.40 1.3757 3 3 3 12 69.07 1.72 1.3599 2 5 1 12 69.07 3.20 1.3599 5 2 1 12 69.82 1.10 1.3471 3 2 4 12 69.82 2.63 1.3471 2 3 4 12 70.19 6.53 1.3409 6 0 2 12 70.27 2.40 1.3396 1 2 5 12 70.27 4.11 1.3396 2 1 5 12 71.16 4.08 1.3250 3 4 2 12 71.16 1.33 1.3250 4 3 2 12 71.60 1.35 1.3179 1 6 0 6 71.60 1.05 1.3179 6 1 0 6 71.75 5.53 1.3155 1 4 4 12 71.75 6.82 1.3155 4 1 4 12 72.04 2.54 1.3109 1 5 3 12 72.04 2.55 1.3109 5 1 3 12 72.93 2.26 1.2972 1 6 1 12 72.93 1.39 1.2972 6 1 1 12 73.07 5.99 1.2949 2 5 2 12 73.07 5.14 1.2949 5 2 2 12 76.34 2.05 1.2474 4 4 0 6 78.36 2.19 1.2203 2 4 4 12 78.36 2.26 1.2203 4 2 4 12 79.01 1.21 1.2119 1 0 6 12 79.57 1.08 1.2047 2 5 3 12 79.57 2.33 1.2047 5 2 3 12 80.86 5.16 1.1887 1 1 6 12 81.14 1.98 1.1853 5 1 4 12 81.14 1.37 1.1853 1 5 4 12 81.57 1.18 1.1802 3 2 5 12 81.57 2.65 1.1802 2 3 5 12 82.41 1.71 1.1702 7 0 2 12 83.26 1.16 1.1604 1 6 3 12 88.89 1.29 1.1009 3 3 5 12 89.11 3.52 1.0989 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.