Stibnite
Kyono A, Kimata M
American Mineralogist 89 (2004) 932-940
Structural variations induced by difference of the inert pair effect
in the stibnite-bismuthinite solid solution series (Sb,Bi)2S3
Sample: Sb1.483Bi.517S3
_database_code_amcsd 0003555
CELL PARAMETERS: 11.3180 3.8830 11.2260 90.000 90.000 90.000
SPACE GROUP: Pnma
X-RAY WAVELENGTH: 1.541838
Cell Volume: 493.358
Density (g/cm3): 5.179
MAX. ABS. INTENSITY / VOLUME**2: 45.21821220
RIR: 2.843
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
11.10 5.10 7.9703 1 0 1 4
15.66 37.06 5.6590 2 0 0 2
15.79 7.09 5.6130 0 0 2 2
17.55 50.83 5.0533 2 0 1 4
17.64 4.06 5.0286 1 0 2 4
22.31 37.31 3.9852 2 0 2 4
24.25 27.34 3.6697 0 1 1 4
24.90 74.17 3.5761 3 0 1 4
25.06 75.56 3.5529 1 0 3 4
25.52 33.27 3.4908 1 1 1 8
27.87 14.15 3.2018 2 1 0 4
28.51 20.09 3.1311 3 0 2 4
28.60 13.85 3.1213 2 0 3 4
29.00 27.65 3.0790 2 1 1 8
29.05 100.00 3.0734 1 1 2 8
32.19 92.98 2.7811 2 1 2 8
32.88 3.83 2.7240 1 0 4 4
33.25 39.97 2.6945 0 1 3 4
33.74 1.98 2.6568 3 0 3 4
34.08 2.88 2.6305 3 1 1 8
34.21 19.73 2.6212 1 1 3 8
35.53 42.48 2.5266 4 0 2 4
35.71 11.54 2.5143 2 0 4 4
36.88 18.58 2.4374 3 1 2 8
39.40 23.76 2.2868 4 1 0 4
39.95 4.05 2.2569 4 0 3 4
40.04 6.22 2.2518 3 0 4 4
40.25 30.74 2.2408 4 1 1 8
40.45 10.97 2.2300 1 1 4 8
40.98 3.32 2.2023 1 0 5 4
41.17 3.19 2.1927 3 1 3 8
42.70 2.71 2.1178 4 1 2 8
42.85 15.31 2.1105 2 1 4 8
43.09 13.81 2.0993 5 0 2 4
43.36 8.37 2.0869 2 0 5 4
45.52 6.28 1.9926 4 0 4 4
46.54 3.52 1.9513 4 1 3 8
46.63 43.53 1.9479 3 1 4 8
46.74 25.44 1.9437 0 1 5 4
46.79 30.65 1.9415 0 2 0 2
46.91 3.33 1.9368 5 0 3 4
47.10 14.96 1.9294 3 0 5 4
47.18 6.82 1.9266 5 1 1 8
47.46 1.98 1.9156 1 1 5 8
48.24 6.89 1.8863 6 0 0 2
48.67 5.29 1.8710 0 0 6 2
48.97 2.72 1.8603 6 0 1 4
49.35 4.78 1.8467 5 1 2 8
49.37 5.14 1.8459 1 0 6 4
49.64 2.87 1.8364 2 2 0 4
50.35 4.48 1.8123 2 2 1 8
51.08 1.02 1.7881 6 0 2 4
51.44 3.43 1.7764 2 0 6 4
51.99 3.68 1.7588 4 0 5 4
52.42 5.68 1.7454 2 2 2 8
52.82 16.10 1.7332 5 1 3 8
53.00 6.59 1.7278 3 1 5 8
53.72 13.39 1.7063 3 2 1 8
53.81 14.08 1.7037 1 2 3 8
54.05 20.50 1.6967 6 1 0 4
54.47 3.90 1.6844 6 0 3 4
54.71 1.40 1.6777 6 1 1 8
55.09 1.80 1.6671 1 1 6 8
55.71 4.08 1.6500 3 2 2 8
55.76 2.97 1.6486 2 2 3 8
58.37 1.18 1.5810 1 2 4 8
59.20 2.43 1.5607 4 0 6 4
59.50 1.41 1.5537 7 0 2 4
59.85 2.00 1.5453 6 1 3 8
59.95 7.76 1.5430 2 0 7 4
60.10 13.07 1.5395 4 2 2 8
60.13 1.95 1.5389 3 1 6 8
60.22 3.59 1.5367 2 2 4 8
62.58 5.20 1.4842 7 0 3 4
62.80 3.52 1.4796 7 1 1 8
63.17 1.50 1.4718 4 2 3 8
63.24 2.33 1.4704 3 2 4 8
63.92 1.31 1.4564 1 2 5 8
64.33 1.98 1.4481 4 1 6 8
64.52 3.46 1.4443 6 0 5 4
64.61 2.12 1.4425 7 1 2 8
64.63 1.37 1.4421 5 0 6 4
65.05 7.60 1.4339 2 1 7 8
65.48 5.76 1.4254 5 2 2 8
65.69 3.45 1.4215 2 2 5 8
66.63 1.40 1.4036 8 0 1 4
66.65 1.63 1.4032 0 0 8 2
66.77 3.58 1.4010 7 0 4 4
67.34 2.81 1.3906 4 2 4 8
68.42 1.55 1.3712 5 2 3 8
68.57 7.04 1.3685 3 2 5 8
69.43 5.41 1.3537 6 1 5 8
69.48 3.31 1.3529 6 2 0 4
69.81 2.59 1.3472 0 2 6 4
70.05 1.34 1.3432 6 2 1 8
70.38 2.56 1.3378 1 2 6 8
71.91 10.58 1.3130 4 1 7 8
72.05 4.42 1.3108 1 1 8 8
72.06 1.81 1.3106 2 2 6 8
72.52 1.92 1.3035 4 2 5 8
73.17 4.82 1.2935 8 1 2 8
74.59 2.28 1.2723 6 2 3 8
75.67 2.18 1.2569 6 1 6 8
75.91 3.40 1.2535 1 3 2 8
76.18 1.15 1.2497 9 0 1 4
76.66 1.75 1.2430 7 1 5 8
76.89 1.24 1.2398 1 0 9 4
77.55 3.77 1.2310 2 3 2 8
78.13 1.74 1.2232 0 3 3 4
78.66 1.58 1.2164 4 2 6 8
79.32 5.07 1.2079 2 2 7 8
79.84 2.53 1.2013 8 1 4 8
80.26 1.06 1.1962 3 3 2 8
80.54 2.01 1.1927 5 0 8 4
80.79 2.05 1.1896 9 1 1 8
80.96 2.68 1.1876 0 1 9 4
81.23 1.41 1.1843 3 0 9 4
81.66 3.61 1.1791 7 2 3 8
81.83 1.50 1.1770 4 3 0 4
82.38 2.03 1.1706 4 3 1 8
82.71 2.60 1.1668 7 1 6 8
83.41 2.48 1.1588 6 2 5 8
84.12 1.16 1.1508 2 3 4 8
84.41 1.97 1.1476 9 0 4 4
85.33 1.01 1.1375 8 2 1 8
85.35 1.24 1.1373 0 2 8 4
85.46 2.71 1.1361 7 2 4 8
86.79 3.89 1.1222 3 3 4 8
86.86 2.27 1.1213 0 3 5 4
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XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs
For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.