Berthierite Periotto B, Balic-Zunic T, Nestola F The Canadian Mineralogist 50 (2012) 201-218 The role of the Sb3+ lone-electron pairs and Fe2+ coordination in the high-pressure behavior of berthierite Note: P = 0.0001 GPa Locality: hydro-thermal vein-type deposit of Herja in the Baia Mare metallogenic area, Romania _database_code_amcsd 0019205 CELL PARAMETERS: 11.4164 14.1705 3.7632 90.000 90.000 90.000 SPACE GROUP: Pnam X-RAY WAVELENGTH: 1.541838 Cell Volume: 608.796 Density (g/cm3): 4.665 MAX. ABS. INTENSITY / VOLUME**2: 26.09270531 RIR: 1.821 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 12.49 33.15 7.0852 0 2 0 2 14.71 4.26 6.0201 1 2 0 4 15.52 3.13 5.7082 2 0 0 2 16.74 6.72 5.2948 2 1 0 4 20.35 44.25 4.3647 1 3 0 4 24.22 97.54 3.6752 3 1 0 4 24.46 58.10 3.6391 2 3 0 4 25.14 20.88 3.5426 0 4 0 2 25.71 28.93 3.4655 1 1 1 8 26.34 43.24 3.3835 1 4 0 4 26.59 1.50 3.3525 3 2 0 4 27.96 100.00 3.1910 1 2 1 8 29.11 36.21 3.0674 2 1 1 8 29.68 53.90 3.0101 2 4 0 4 30.16 9.93 2.9634 3 3 0 4 31.14 90.51 2.8721 2 2 1 8 33.86 1.37 2.6474 4 2 0 4 34.10 92.57 2.6293 3 1 1 8 34.28 91.21 2.6160 2 3 1 8 34.59 2.70 2.5930 3 4 0 4 35.36 30.09 2.5384 2 5 0 4 35.68 19.64 2.5160 1 4 1 8 35.87 10.73 2.5032 3 2 1 8 36.79 1.84 2.4428 4 3 0 4 38.10 2.95 2.3617 0 6 0 2 38.29 6.48 2.3506 2 4 1 8 38.67 4.24 2.3282 3 3 1 8 38.94 6.24 2.3128 1 6 0 4 39.63 6.85 2.2741 4 0 1 4 39.65 10.82 2.2730 3 5 0 4 39.82 4.44 2.2639 0 5 1 4 40.00 1.60 2.2542 5 1 0 4 40.16 23.26 2.2453 4 1 1 8 40.59 1.14 2.2225 4 4 0 4 40.63 17.45 2.2207 1 5 1 8 41.37 5.62 2.1823 2 6 0 4 41.55 28.31 2.1732 5 2 0 4 41.71 16.47 2.1653 4 2 1 8 42.33 1.57 2.1352 3 4 1 8 42.98 4.31 2.1044 2 5 1 8 44.05 3.47 2.0557 5 3 0 4 44.20 31.00 2.0490 4 3 1 8 45.08 17.28 2.0110 4 5 0 4 45.18 15.02 2.0067 3 6 0 4 45.51 5.55 1.9933 1 7 0 4 46.06 3.59 1.9704 1 6 1 8 46.69 4.53 1.9456 3 5 1 8 47.37 26.38 1.9192 5 4 0 4 47.51 3.24 1.9137 4 4 1 8 47.66 2.49 1.9079 2 7 0 4 47.80 2.51 1.9027 6 0 0 2 48.20 13.77 1.8879 2 6 1 8 48.36 8.56 1.8819 5 2 1 8 48.37 44.96 1.8816 0 0 2 2 50.16 1.77 1.8186 0 2 2 4 50.60 27.51 1.8041 5 3 1 8 51.24 35.49 1.7828 0 7 1 4 51.39 1.04 1.7780 5 5 0 4 51.53 2.93 1.7737 4 5 1 8 51.62 21.72 1.7707 3 6 1 8 51.91 22.29 1.7614 1 7 1 8 53.00 5.39 1.7279 1 3 2 8 53.60 6.38 1.7097 5 4 1 8 53.88 3.66 1.7017 2 7 1 8 54.00 16.76 1.6980 6 0 1 4 54.22 2.18 1.6917 2 8 0 4 54.81 17.62 1.6749 3 1 2 8 54.93 10.82 1.6714 2 3 2 8 55.28 4.11 1.6618 0 4 2 4 55.91 8.68 1.6444 1 4 2 8 56.15 1.43 1.6381 4 6 1 8 56.82 6.09 1.6202 7 1 0 4 57.31 3.30 1.6076 5 5 1 8 57.38 1.83 1.6059 3 8 0 4 57.69 4.92 1.5979 6 3 1 8 57.79 12.38 1.5955 2 4 2 8 58.03 10.24 1.5894 7 2 0 4 58.07 2.34 1.5885 3 3 2 8 58.42 1.55 1.5797 6 5 0 4 59.24 8.80 1.5597 1 9 0 4 59.95 6.79 1.5430 2 8 1 8 60.46 5.95 1.5312 6 4 1 8 61.33 9.53 1.5116 2 5 2 8 61.62 9.02 1.5050 4 8 0 4 62.40 4.28 1.4882 7 1 1 8 63.18 1.18 1.4717 0 6 2 4 63.54 3.41 1.4641 7 2 1 8 63.77 2.43 1.4596 1 6 2 8 63.99 2.52 1.4549 3 9 0 4 64.27 4.31 1.4494 3 5 2 8 65.50 2.22 1.4251 2 6 2 8 65.63 12.02 1.4225 5 2 2 8 65.77 1.62 1.4199 8 1 0 4 66.49 1.53 1.4063 1 10 0 4 66.55 4.72 1.4052 5 7 1 8 66.85 2.04 1.3995 5 8 0 4 66.88 1.90 1.3990 8 2 0 4 67.48 1.47 1.3880 5 3 2 8 67.57 4.27 1.3864 6 7 0 4 68.00 2.71 1.3787 6 6 1 8 68.01 4.52 1.3785 7 4 1 8 68.19 2.33 1.3753 2 10 0 4 68.26 7.98 1.3740 4 5 2 8 68.34 7.09 1.3726 3 6 2 8 68.59 2.70 1.3683 1 7 2 8 68.71 4.12 1.3661 8 3 0 4 70.03 13.29 1.3436 5 4 2 8 70.12 1.60 1.3420 7 6 0 4 70.26 1.23 1.3397 2 7 2 8 70.37 1.26 1.3379 6 0 2 4 70.97 1.38 1.3280 3 10 0 4 71.26 5.54 1.3233 7 5 1 8 72.99 2.02 1.2962 5 9 0 4 73.28 1.33 1.2917 2 10 1 8 73.79 2.51 1.2841 8 3 1 8 74.75 1.12 1.2700 7 7 0 4 74.80 2.16 1.2692 4 10 0 4 75.16 2.25 1.2641 7 6 1 8 75.58 1.31 1.2580 2 8 2 8 75.99 6.85 1.2523 3 10 1 8 76.25 1.23 1.2487 8 4 1 8 76.73 1.01 1.2421 1 1 3 8 77.77 3.81 1.2280 1 2 3 8 77.79 4.04 1.2278 7 1 2 8 77.96 5.93 1.2255 5 9 1 8 78.27 1.22 1.2215 3 8 2 8 78.33 1.43 1.2206 2 1 3 8 78.47 6.39 1.2188 0 11 1 4 78.83 6.88 1.2142 7 2 2 8 78.92 1.01 1.2130 6 9 0 4 79.01 1.41 1.2119 1 11 1 8 79.17 1.08 1.2099 6 5 2 8 79.37 3.92 1.2073 2 2 3 8 79.37 2.98 1.2072 8 5 1 8 79.88 6.08 1.2008 1 9 2 8 80.13 6.39 1.1977 9 1 1 8 80.99 4.99 1.1872 3 1 3 8 81.09 5.04 1.1859 2 3 3 8 81.16 1.41 1.1851 9 2 1 8 81.91 1.26 1.1762 1 4 3 8 81.98 6.73 1.1753 4 8 2 8 83.24 1.14 1.1607 3 11 1 8 83.62 1.02 1.1564 2 12 0 4 84.10 1.96 1.1510 3 9 2 8 84.68 1.84 1.1446 4 1 3 8 84.95 1.03 1.1416 10 0 0 2 84.98 1.36 1.1413 1 5 3 8 85.29 1.17 1.1380 10 1 0 4 85.70 1.36 1.1336 4 2 3 8 85.72 1.33 1.1334 8 1 2 8 86.31 1.51 1.1271 10 2 0 4 86.38 1.35 1.1264 1 10 2 8 86.71 1.71 1.1230 5 8 2 8 86.74 1.60 1.1227 8 2 2 8 87.24 1.98 1.1175 9 6 0 4 87.37 3.59 1.1162 6 7 2 8 87.40 3.05 1.1159 4 3 3 8 87.57 2.06 1.1141 8 7 1 8 87.95 2.02 1.1103 2 10 2 8 88.32 3.78 1.1066 9 5 1 8 88.43 3.58 1.1054 8 3 2 8 89.75 1.44 1.0926 7 6 2 8 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.