Bonazziite Bindi L, Pratesi G, Muniz-Miranda M, Zoppi M, Chelazzi L, Lepore G O, Menchetti S Mineralogical Magazine 79 (2015) 121-131 From ancient pigments to modern optoelectronic applications of arsenic sulfides: bonazziite, the natural analogue of beta-As4S4 from Khaidarkan deposit, Kyrgyzstan Locality: Fergana Valley, Alai Range, Osh Oblast, Kyrgyzstan _database_code_amcsd 0020633 CELL PARAMETERS: 9.9560 9.3080 8.8690 90.000 102.550 90.000 SPACE GROUP: C2/c X-RAY WAVELENGTH: 1.541838 Cell Volume: 802.257 Density (g/cm3): 3.543 MAX. ABS. INTENSITY / VOLUME**2: 24.70174451 RIR: 2.270 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 13.17 9.95 6.7221 1 1 0 4 15.43 100.00 5.7441 -1 1 1 4 17.88 31.37 4.9605 1 1 1 4 18.26 23.26 4.8591 2 0 0 2 19.07 13.09 4.6540 0 2 0 2 21.68 72.85 4.0992 0 2 1 4 22.70 39.53 3.9171 -1 1 2 4 24.39 1.05 3.6499 -2 0 2 2 26.11 4.48 3.4133 1 1 2 4 26.52 5.44 3.3610 2 2 0 4 28.15 25.45 3.1696 0 2 2 4 29.19 45.34 3.0594 3 1 0 4 29.93 23.12 2.9854 2 2 1 4 30.24 6.66 2.9557 1 3 0 4 30.50 19.64 2.9312 2 0 2 2 31.14 63.21 2.8720 -2 2 2 4 31.33 14.74 2.8554 -1 3 1 4 31.86 28.90 2.8091 -1 1 3 4 32.18 2.47 2.7819 -3 1 2 4 32.65 8.02 2.7423 1 3 1 4 32.99 7.01 2.7148 3 1 1 4 35.63 5.17 2.5197 -1 3 2 4 35.66 18.52 2.5180 1 1 3 4 36.22 6.62 2.4803 2 2 2 4 37.00 6.47 2.4295 4 0 0 2 37.92 31.96 2.3728 -2 2 3 4 37.98 6.75 2.3691 1 3 2 4 38.34 3.43 2.3475 -4 0 2 2 40.02 7.17 2.2529 -3 3 1 4 40.13 7.74 2.2472 0 4 1 4 40.25 19.78 2.2407 3 3 0 4 41.20 5.20 2.1912 -4 2 1 4 41.73 2.33 2.1643 0 0 4 2 41.84 5.77 2.1591 -2 0 4 2 41.88 3.60 2.1569 -1 1 4 4 41.95 7.34 2.1537 4 2 0 4 42.30 10.23 2.1366 -1 3 3 4 42.55 4.25 2.1245 -3 3 2 4 43.10 5.83 2.0987 2 4 0 4 43.16 1.29 2.0960 -4 2 2 4 43.20 5.34 2.0942 3 3 1 4 43.40 15.61 2.0850 -2 4 1 4 44.34 2.39 2.0429 2 2 3 4 45.35 2.49 1.9998 1 3 3 4 45.94 1.47 1.9753 1 1 4 4 46.14 5.94 1.9674 -3 1 4 4 46.27 7.66 1.9621 -2 4 2 4 46.65 1.28 1.9471 -5 1 1 4 47.49 9.36 1.9147 -3 3 3 4 47.55 2.76 1.9124 3 1 3 4 47.57 4.44 1.9115 -4 2 3 4 47.96 1.75 1.8967 -5 1 2 4 49.70 5.40 1.8344 2 0 4 2 49.88 11.01 1.8284 1 5 0 4 49.98 4.98 1.8250 -4 0 4 2 50.05 1.23 1.8225 2 4 2 4 50.38 3.26 1.8114 0 4 3 4 50.60 1.79 1.8039 -1 3 4 4 50.86 10.89 1.7952 4 2 2 4 51.31 6.13 1.7805 5 1 1 4 51.61 10.27 1.7709 -5 1 3 4 54.61 4.37 1.6805 4 4 0 4 54.78 2.90 1.6757 -5 3 1 4 55.34 14.98 1.6601 1 5 2 4 55.35 10.41 1.6599 -3 1 5 4 55.58 5.71 1.6535 3 3 3 4 56.14 1.34 1.6383 -6 0 2 2 56.59 2.61 1.6263 2 4 3 4 56.73 5.05 1.6228 0 2 5 4 56.84 10.32 1.6197 6 0 0 2 56.85 3.84 1.6195 5 1 2 4 56.87 3.83 1.6189 1 1 5 4 56.94 1.92 1.6173 3 1 4 4 57.41 1.98 1.6052 4 4 1 4 58.17 6.10 1.5858 4 2 3 4 58.22 2.54 1.5848 0 4 4 4 58.86 1.52 1.5690 -3 5 2 4 59.33 2.00 1.5576 -4 4 3 4 59.85 3.13 1.5454 -6 2 2 4 60.12 6.06 1.5390 -1 3 5 4 61.96 1.02 1.4976 -4 2 5 4 62.19 2.08 1.4927 4 4 2 4 63.92 1.58 1.4563 -1 1 6 4 63.94 2.52 1.4560 6 2 1 4 64.08 2.21 1.4531 5 3 2 4 64.10 1.41 1.4529 2 2 5 4 64.62 1.46 1.4423 -5 1 5 4 65.36 2.62 1.4277 -2 6 2 4 66.73 1.28 1.4017 -2 4 5 4 67.39 4.63 1.3896 3 1 5 4 67.42 2.28 1.3891 0 4 5 4 67.97 1.86 1.3791 -4 0 6 2 68.67 1.01 1.3667 -3 5 4 4 68.69 3.74 1.3664 0 6 3 4 69.16 1.63 1.3583 -7 1 3 4 69.61 2.06 1.3506 -6 4 1 4 69.98 1.30 1.3444 5 5 0 4 70.10 4.92 1.3423 -5 5 2 4 70.91 1.47 1.3290 5 3 3 4 72.22 4.65 1.3082 -4 4 5 4 72.24 2.62 1.3078 2 0 6 2 73.76 1.05 1.2846 -6 2 5 4 73.97 3.04 1.2815 2 6 3 4 74.20 2.62 1.2780 2 4 5 4 76.37 2.60 1.2470 -4 6 3 4 76.53 1.20 1.2448 -2 4 6 4 77.01 1.07 1.2383 -3 1 7 4 77.51 1.42 1.2315 3 5 4 4 77.62 2.26 1.2301 3 7 0 4 79.95 1.14 1.1999 -8 2 2 4 81.71 2.30 1.1786 -8 2 3 4 85.51 2.09 1.1356 -7 3 5 4 86.57 1.34 1.1244 4 4 5 4 87.49 1.56 1.1149 1 3 7 4 87.51 1.20 1.1147 2 8 1 4 87.69 2.53 1.1129 7 5 0 4 87.90 1.36 1.1108 1 5 6 4 88.81 1.09 1.1018 -6 6 3 4 89.32 1.05 1.0968 5 3 5 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.