Leadhillite
Bindi L, Menchetti S
American Mineralogist 90 (2005) 1641-1647
Structural changes accompanying the phase transformation between leadhillite
and susannite: a structural study by means of in situ high-temperature single-
crystal X-ray diffraction
Sample: Chah Mileh Mine, Anarak District, Esfahan Province, Iran
Sample: T = 25 C
_database_code_amcsd 0003938
CELL PARAMETERS: 9.1040 20.7920 11.5770 90.000 90.500 90.000
SPACE GROUP: P2_1/a
X-RAY WAVELENGTH: 1.541838
Cell Volume: 2191.331
Density (g/cm3): 6.527
MAX. ABS. INTENSITY / VOLUME**2: 101.9240965
RIR: 5.084
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
7.64 24.78 11.5766 0 0 1 2
13.03 4.18 6.7923 -1 1 1 4
13.13 2.73 6.7410 1 1 1 4
14.90 4.37 5.9465 0 3 1 4
15.31 4.97 5.7883 0 0 2 2
18.59 3.02 4.7730 -1 1 2 4
18.73 1.58 4.7374 1 1 2 4
19.50 18.04 4.5518 2 0 0 2
19.67 31.31 4.5140 1 4 0 4
19.99 5.10 4.4427 0 3 2 4
20.91 4.90 4.2488 -2 0 1 2
21.09 1.19 4.2118 -1 4 1 4
21.16 8.75 4.1994 1 4 1 4
22.72 4.56 3.9136 0 5 1 4
23.05 2.00 3.8589 0 0 3 2
24.58 3.26 3.6223 -2 3 1 4
24.68 4.34 3.6067 2 3 1 4
24.78 55.78 3.5933 -2 0 2 2
24.96 52.13 3.5670 -1 4 2 4
24.99 26.34 3.5629 2 0 2 2
25.07 100.00 3.5521 1 4 2 4
26.39 7.99 3.3772 0 5 2 4
27.97 4.54 3.1900 -2 3 2 4
28.16 4.74 3.1687 2 3 2 4
29.09 10.39 3.0701 2 5 0 4
29.75 6.65 3.0027 3 1 0 4
30.23 1.96 2.9562 -2 0 3 2
30.41 42.81 2.9394 -1 4 3 4
30.50 24.28 2.9309 2 0 3 2
30.54 4.70 2.9269 1 4 3 4
30.90 19.00 2.8941 0 0 4 2
31.69 9.21 2.8238 1 7 0 4
32.47 1.36 2.7572 2 6 0 4
32.67 1.35 2.7410 -1 1 4 4
32.84 1.65 2.7274 1 1 4 4
32.94 1.04 2.7192 -2 3 3 4
33.75 1.46 2.6561 3 1 2 4
34.22 56.64 2.6207 3 4 0 4
34.51 24.18 2.5990 0 8 0 2
35.05 3.00 2.5601 -3 4 1 4
35.17 2.44 2.5518 3 4 1 4
35.33 1.44 2.5406 -1 7 2 4
35.40 3.06 2.5359 0 8 1 4
36.82 4.94 2.4412 -1 4 4 4
36.95 3.67 2.4327 2 0 4 2
37.32 1.27 2.4094 -2 5 3 4
37.54 2.25 2.3956 2 5 3 4
37.80 2.27 2.3798 -3 1 3 4
37.87 1.24 2.3755 0 5 4 4
38.13 1.03 2.3599 3 1 3 4
38.90 21.19 2.3153 0 0 5 2
38.96 1.44 2.3116 -2 3 4 4
39.49 1.37 2.2818 -1 7 3 4
39.60 3.18 2.2759 4 0 0 2
39.60 2.70 2.2759 1 7 3 4
39.94 6.13 2.2570 2 8 0 4
40.28 4.16 2.2392 1 9 0 4
40.32 1.65 2.2369 -4 0 1 2
40.76 4.19 2.2135 2 8 1 4
41.07 1.28 2.1976 1 9 1 4
41.77 2.74 2.1623 4 3 0 4
41.81 1.15 2.1604 3 4 3 4
42.46 1.89 2.1287 -4 3 1 4
42.56 7.74 2.1244 -4 0 2 2
42.59 1.32 2.1227 3 7 0 4
42.82 11.08 2.1118 4 0 2 2
42.95 16.70 2.1059 -2 8 2 4
43.08 12.43 2.0997 2 8 2 4
43.29 4.05 2.0899 -1 9 2 4
43.71 7.10 2.0710 -2 0 5 2
44.03 13.77 2.0565 1 4 5 4
44.87 2.44 2.0201 4 3 2 4
44.91 1.06 2.0184 1 7 4 4
45.42 3.89 1.9968 -3 7 2 4
46.08 1.31 1.9699 -4 5 1 4
46.13 3.73 1.9679 -4 0 3 2
46.20 1.36 1.9649 4 5 1 4
46.50 1.76 1.9529 4 0 3 2
46.53 4.78 1.9519 -2 8 3 4
46.58 6.16 1.9499 -3 4 4 4
46.71 6.33 1.9446 2 8 3 4
46.95 6.36 1.9353 3 4 4 4
46.96 2.18 1.9350 1 9 3 4
46.99 4.96 1.9337 0 8 4 4
48.06 1.62 1.8931 -4 3 3 4
48.10 2.43 1.8918 -4 5 2 4
48.34 2.07 1.8829 4 5 2 4
49.11 1.18 1.8551 3 7 3 4
49.15 1.20 1.8538 -2 5 5 4
49.44 1.38 1.8434 2 5 5 4
49.50 1.16 1.8412 -3 1 5 4
50.81 2.52 1.7968 0 11 2 4
50.94 1.51 1.7928 -1 7 5 4
51.22 1.22 1.7835 -2 8 4 4
51.45 1.05 1.7761 2 8 4 4
51.67 2.05 1.7692 1 9 4 4
52.13 1.10 1.7546 -3 9 2 4
52.30 3.13 1.7493 3 9 2 4
52.41 1.21 1.7457 2 11 0 4
52.54 9.98 1.7417 -3 4 5 4
52.63 1.63 1.7392 -4 3 4 4
52.76 2.21 1.7351 -5 1 2 4
52.97 9.26 1.7288 0 8 5 4
52.97 10.13 1.7287 3 4 5 4
53.31 1.45 1.7184 5 4 0 4
53.52 1.48 1.7122 4 8 0 4
54.01 1.18 1.6977 5 4 1 4
54.09 1.38 1.6954 -4 8 1 4
54.48 2.22 1.6844 -1 12 1 4
54.99 1.41 1.6698 2 11 2 4
55.67 3.50 1.6510 -5 4 2 4
55.90 2.66 1.6448 -4 8 2 4
55.94 3.36 1.6436 5 4 2 4
56.12 2.89 1.6390 4 8 2 4
56.17 1.53 1.6375 4 5 4 4
56.31 1.92 1.6337 -1 12 2 4
56.37 1.93 1.6323 1 12 2 4
56.85 2.07 1.6197 -2 8 5 4
56.99 1.43 1.6160 4 0 5 2
57.11 1.18 1.6127 2 8 5 4
57.17 1.39 1.6113 -1 9 5 4
58.63 1.69 1.5746 -5 4 3 4
58.84 1.12 1.5694 -3 7 5 4
58.86 2.18 1.5689 -4 8 3 4
59.02 2.36 1.5650 5 4 3 4
59.18 1.51 1.5613 4 8 3 4
59.28 2.68 1.5588 -2 0 7 2
59.30 1.76 1.5583 -1 12 3 4
59.38 1.78 1.5564 1 12 3 4
59.44 7.95 1.5550 -1 4 7 4
59.62 5.44 1.5507 1 4 7 4
59.65 4.26 1.5500 2 0 7 2
60.01 1.63 1.5416 0 13 2 4
61.07 2.06 1.5173 6 0 0 2
61.45 1.67 1.5089 2 13 0 4
61.64 2.80 1.5047 3 12 0 4
61.76 1.05 1.5021 -5 7 2 4
62.01 1.02 1.4965 5 7 2 4
62.18 1.27 1.4929 -3 12 1 4
62.65 1.19 1.4829 -5 4 4 4
62.68 1.29 1.4822 6 3 0 4
63.29 1.12 1.4694 4 8 4 4
63.45 1.21 1.4661 1 12 4 4
64.03 1.15 1.4541 4 11 0 4
65.25 1.18 1.4300 5 9 0 4
70.04 1.35 1.3435 -4 0 7 2
70.44 2.27 1.3368 -2 8 7 4
70.71 1.26 1.3324 4 0 7 2
70.77 2.27 1.3313 2 8 7 4
72.08 1.81 1.3103 6 8 0 4
73.64 1.44 1.2863 0 0 9 2
75.15 1.68 1.2642 -3 12 5 4
75.50 1.11 1.2592 3 12 5 4
76.73 1.11 1.2420 2 16 1 4
80.48 1.09 1.1934 -4 8 7 4
81.03 1.53 1.1867 5 4 7 4
83.46 1.19 1.1582 -3 4 9 4
83.94 1.05 1.1528 0 8 9 4
84.08 1.46 1.1513 3 4 9 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.