Suolunite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from the powder pattern for R060917 Ma Z, Shi N, Mou G, Liao L Chinese Science Bulletin 44 (1999) 2125-2130 Crystal structure refinement of suolunite and its significance to the cement techniques Locality: Geological Museum of China CELL PARAMETERS: 19.82051 6.003398 11.15013 90.00000 90.00000 90.00000 SPACE GROUP: Fd2d X-RAY WAVELENGTH: 1.541838 2-THETA INTENSITY D-SPACING H K L 17.39 25.96 5.1074 1 1 1 17.93 8.17 4.9551 4 0 0 21.55 100.00 4.1275 3 1 1 24.05 4.73 3.7037 4 0 2 28.16 68.48 3.1714 5 1 1 28.62 3.42 3.1207 1 1 3 31.15 3.74 2.8728 2 2 0 31.39 51.98 2.8508 3 1 3 31.49 8.77 2.8420 6 0 2 32.13 2.82 2.7875 0 0 4 33.41 41.83 2.6834 2 0 4 33.93 25.74 2.6430 0 2 2 35.15 31.70 2.5537 2 2 2 35.99 23.28 2.4960 7 1 1 36.27 8.36 2.4776 8 0 0 36.37 7.96 2.4710 5 1 3 37.01 11.33 2.4295 4 0 4 38.62 16.69 2.3320 4 2 2 39.82 1.05 2.2641 8 0 2 40.62 22.69 2.2215 6 2 0 42.89 16.94 2.1088 7 1 3 43.54 9.08 2.0789 1 1 5 43.87 13.75 2.0637 6 2 2 44.57 9.89 2.0329 9 1 1 45.33 8.28 2.0006 2 2 4 45.51 26.95 1.9931 3 1 5 46.33 1.11 1.9600 1 3 1 48.19 2.19 1.8884 4 2 4 48.21 24.76 1.8876 3 3 1 48.76 1.66 1.8675 10 0 2 49.20 19.35 1.8518 8 0 4 49.28 12.24 1.8491 5 1 5 49.93 1.04 1.8265 2 0 6 50.49 4.18 1.8075 8 2 2 51.83 6.91 1.7639 5 3 1 52.11 1.33 1.7551 1 3 3 53.74 9.59 1.7055 11 1 1 53.84 2.46 1.7025 3 3 3 54.56 8.36 1.6818 7 1 5 55.55 1.13 1.6540 10 2 0 55.64 2.95 1.6517 12 0 0 56.94 5.03 1.6169 7 3 1 57.00 7.70 1.6153 10 0 4 57.21 10.67 1.6101 5 3 3 58.17 14.31 1.5857 10 2 2 58.40 8.25 1.5801 0 2 6 58.56 2.19 1.5760 8 2 4 59.00 1.05 1.5653 11 1 3 59.21 1.73 1.5603 2 2 6 60.28 2.02 1.5350 1 1 7 61.60 4.42 1.5054 4 2 6 61.80 6.15 1.5008 0 4 0 61.87 1.96 1.4994 3 1 7 62.46 1.07 1.4866 8 0 6 64.08 5.18 1.4529 3 3 5 64.96 4.79 1.4352 5 1 7 65.02 1.76 1.4340 2 4 2 65.62 4.34 1.4224 10 2 4 65.69 3.24 1.4210 12 0 4 66.77 4.75 1.4007 12 2 2 67.12 6.02 1.3942 5 3 5 67.89 3.71 1.3802 2 0 8 68.14 1.13 1.3758 9 3 3 68.29 6.75 1.3732 13 1 3 69.29 1.68 1.3557 10 0 6 70.69 14.17 1.3322 8 2 6 71.00 1.35 1.3272 6 4 2 71.35 4.90 1.3215 0 4 4 71.56 2.54 1.3182 7 3 5 72.08 5.04 1.3099 2 4 4 73.79 4.97 1.2837 8 4 0 73.76 3.47 1.2841 6 0 8 73.91 6.07 1.2819 15 1 1 74.25 2.38 1.2769 4 4 4 77.45 1.57 1.2318 13 1 5 77.82 3.35 1.2269 6 4 4 77.99 2.20 1.2247 3 3 7 79.04 1.13 1.2111 1 1 9 79.46 1.41 1.2057 13 3 1 80.81 1.42 1.1889 5 3 7 81.99 3.46 1.1748 3 5 1 82.35 1.75 1.1705 11 1 7 82.74 4.15 1.1660 8 4 4 83.24 5.76 1.1602 5 1 9 83.88 3.35 1.1529 13 3 3 84.33 2.44 1.1480 11 3 5 84.78 1.50 1.1431 5 5 1 84.90 1.30 1.1418 12 2 6 85.00 1.06 1.1407 7 3 7 85.05 4.04 1.1401 10 0 8 86.37 1.08 1.1260 8 2 8 86.78 1.61 1.1217 16 2 2 87.25 3.21 1.1169 15 1 5 87.85 5.61 1.1108 12 4 0 88.94 1.22 1.1000 7 5 1 88.99 4.46 1.0995 10 4 4 89.16 3.67 1.0979 5 5 3 89.21 2.46 1.0973 15 3 1 89.57 1.38 1.0938 17 1 3 89.57 1.38 1.0938 17 1 3 XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.