Fourmarierite
Li Y, Burns P C
The Canadian Mineralogist 38 (2000) 737-749
Investigations of crystal-chemical variability in lead uranyl oxide
hydrates. II. Fourmarierite
Note: sample CMNMC 81101
Locality: Shaba, Democratic Republic of Congo
_database_code_amcsd 0005682
CELL PARAMETERS: 14.0260 16.4760 14.3820 90.000 90.000 90.000
SPACE GROUP: Bb2_1m
X-RAY WAVELENGTH: 1.541838
Cell Volume: 3323.571
Density (g/cm3): 5.915
MAX. ABS. INTENSITY / VOLUME**2: 153.5262530
RIR: 8.452
RIR based on corundum from Acta Crystallographica A38 (1982) 733-739
2-THETA INTENSITY D-SPACING H K L Multiplicity
10.32 9.34 8.5744 1 1 1 4
10.74 2.08 8.2380 0 2 0 1
12.31 100.00 7.1910 0 0 2 2
12.62 3.34 7.0130 2 0 0 2
13.72 11.30 6.4528 2 1 0 2
13.90 5.27 6.3689 1 2 1 4
17.67 3.38 5.0207 2 0 2 4
18.41 4.02 4.8184 1 3 1 4
20.30 16.75 4.3736 1 1 3 4
20.54 3.47 4.3239 2 3 0 2
20.72 4.16 4.2872 2 2 2 4
21.57 3.54 4.1190 0 4 0 1
22.73 7.10 3.9128 3 2 1 4
24.02 2.14 3.7056 2 3 2 4
24.76 43.55 3.5955 0 0 4 2
24.91 2.23 3.5742 0 4 2 2
25.07 45.17 3.5517 2 4 0 2
25.40 20.40 3.5065 4 0 0 2
25.47 2.15 3.4975 1 3 3 4
25.98 2.42 3.4297 4 1 0 2
27.19 2.48 3.2801 3 1 3 4
28.02 97.41 3.1845 2 4 2 4
28.32 39.29 3.1518 4 0 2 4
28.42 3.53 3.1408 2 1 4 4
28.51 4.55 3.1309 1 5 1 4
28.79 2.94 3.1009 3 2 3 4
28.84 7.66 3.0956 4 1 2 4
29.96 1.33 2.9824 2 5 0 2
32.38 1.64 2.7646 2 3 4 4
32.61 2.02 2.7460 0 6 0 1
32.76 11.98 2.7336 4 3 2 4
33.07 1.85 2.7087 0 4 4 2
34.34 1.17 2.6113 5 2 1 4
35.10 1.05 2.5570 2 6 0 2
35.53 17.33 2.5268 2 4 4 4
35.77 8.97 2.5103 4 0 4 4
35.82 2.35 2.5070 1 3 5 4
37.52 2.67 2.3970 0 0 6 2
38.33 1.49 2.3482 3 2 5 4
38.77 1.40 2.3229 5 2 3 4
38.91 4.21 2.3145 6 1 0 2
39.74 1.28 2.2682 2 0 6 4
40.31 1.68 2.2374 3 3 5 4
40.42 4.18 2.2314 2 7 0 2
40.58 1.00 2.2231 6 0 2 4
40.96 1.84 2.2032 6 1 2 4
41.28 1.23 2.1868 2 2 6 4
41.37 2.14 2.1823 0 6 4 2
41.78 1.66 2.1620 4 6 0 2
42.01 1.41 2.1509 6 3 0 2
42.20 3.56 2.1416 1 5 5 4
42.59 1.95 2.1230 3 6 3 4
43.72 2.80 2.0704 4 6 2 4
43.94 1.57 2.0607 6 3 2 4
43.97 7.62 2.0595 0 8 0 1
44.57 13.18 2.0331 6 4 0 2
44.93 5.13 2.0176 1 1 7 4
45.50 1.36 1.9935 5 1 5 4
45.66 18.16 1.9869 2 4 6 4
45.83 7.49 1.9799 0 8 2 2
45.86 7.67 1.9788 4 0 6 4
46.21 1.73 1.9647 4 1 6 4
46.41 8.85 1.9564 6 4 2 4
46.67 3.39 1.9461 6 1 4 4
47.21 1.13 1.9253 3 7 3 4
47.70 1.14 1.9066 6 5 0 2
47.70 1.71 1.9065 1 3 7 4
47.73 2.33 1.9054 2 8 2 4
47.98 3.02 1.8960 2 7 4 4
48.25 1.52 1.8861 5 3 5 4
48.26 1.37 1.8859 4 7 2 4
48.73 1.54 1.8688 3 1 7 4
48.93 3.52 1.8617 4 3 6 4
49.18 1.56 1.8528 4 6 4 4
49.37 1.38 1.8458 6 3 4 4
49.46 1.91 1.8429 6 5 2 4
50.53 1.08 1.8064 1 7 5 4
50.56 1.56 1.8051 5 4 5 4
50.79 4.37 1.7977 0 0 8 2
51.11 6.72 1.7871 0 8 4 2
51.46 5.43 1.7758 4 8 0 2
51.65 11.61 1.7697 6 4 4 4
52.49 1.32 1.7434 8 1 0 2
53.12 7.87 1.7241 4 8 2 4
53.82 3.66 1.7034 8 0 2 4
54.98 2.34 1.6702 8 3 0 2
55.39 2.38 1.6586 6 7 0 2
56.57 2.87 1.6269 8 3 2 4
56.98 2.30 1.6162 6 7 2 4
57.40 1.04 1.6054 4 6 6 4
57.45 3.81 1.6040 2 4 8 4
57.62 2.10 1.5998 4 0 8 4
57.92 5.31 1.5922 4 8 4 4
58.87 1.42 1.5687 8 1 4 4
59.00 3.34 1.5655 2 10 2 4
59.14 2.05 1.5621 0 8 6 2
59.63 2.07 1.5505 6 4 6 4
60.14 1.07 1.5385 1 7 7 4
60.72 1.52 1.5253 1 3 9 4
61.19 2.66 1.5148 8 3 4 4
61.58 2.55 1.5061 6 7 4 4
63.29 1.26 1.4694 3 7 7 4
63.51 1.10 1.4648 2 10 4 4
65.23 1.08 1.4304 1 5 9 4
65.40 2.82 1.4269 4 8 6 4
66.02 1.27 1.4151 8 0 6 4
68.38 1.43 1.3719 10 1 2 4
68.47 1.11 1.3704 8 3 6 4
69.39 1.85 1.3543 0 8 8 2
69.48 1.71 1.3528 4 11 2 4
69.80 1.14 1.3474 2 12 0 2
69.84 2.86 1.3467 6 4 8 4
69.87 1.07 1.3462 5 3 9 4
70.66 2.66 1.3331 2 4 10 4
70.67 1.57 1.3330 2 10 6 4
70.81 1.10 1.3306 4 0 10 4
71.20 2.59 1.3244 2 12 2 4
71.73 1.04 1.3158 5 4 9 4
71.94 2.08 1.3126 8 8 2 4
75.21 1.59 1.2634 4 8 8 4
75.32 1.52 1.2617 2 12 4 4
75.36 1.32 1.2612 6 10 4 4
80.89 2.60 1.1883 10 7 2 4
82.04 1.41 1.1746 2 12 6 4
82.59 1.14 1.1682 6 12 2 4
82.75 1.14 1.1663 8 8 6 4
86.53 1.34 1.1248 8 11 2 4
86.56 1.04 1.1245 6 12 4 4
88.73 1.18 1.1025 4 14 2 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.