Lawsonite Pawley A R, Allan D R Mineralogical Magazine 65 (2001) 41-58 A high-pressure study of lawsonite using angle-dispersive powder-diffraction methods with synchrotron radiation Note: Run #BN90, P = 11.9 GPa Locality: synthetic _database_code_amcsd 0018955 CELL PARAMETERS: 5.1970 12.8630 5.6810 90.000 124.480 90.000 SPACE GROUP: P2_1/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 313.053 Density (g/cm3): 3.335 MAX. ABS. INTENSITY / VOLUME**2: 5.845282027 RIR: 0.571 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 13.77 25.39 6.4315 0 2 0 2 18.54 29.18 4.7864 -1 0 1 2 18.95 8.77 4.6830 0 0 1 2 19.79 15.32 4.4859 -1 1 1 4 20.18 5.92 4.4004 0 1 1 4 20.73 1.28 4.2840 1 0 0 2 21.87 27.85 4.0645 1 1 0 4 23.16 8.83 3.8398 -1 2 1 4 23.50 2.00 3.7857 0 2 1 4 24.97 49.12 3.5654 1 2 0 4 27.74 1.07 3.2157 0 4 0 2 27.94 16.56 3.1937 -1 3 1 4 28.22 8.96 3.1624 0 3 1 4 31.50 23.35 2.8397 -1 0 2 2 33.57 63.02 2.6693 -1 4 1 4 33.81 32.64 2.6509 0 4 1 4 34.53 49.56 2.5978 -1 2 2 4 34.82 32.54 2.5762 -2 0 1 2 34.89 100.00 2.5718 1 4 0 4 35.52 27.01 2.5276 1 0 1 2 35.54 1.63 2.5260 -2 1 1 4 37.58 49.47 2.3932 -2 0 2 2 37.61 17.50 2.3915 -2 2 1 4 38.01 19.73 2.3675 -1 3 2 4 38.25 7.60 2.3528 -2 1 2 4 38.26 11.74 2.3525 1 2 1 4 39.99 12.36 2.2548 0 5 1 4 40.21 2.59 2.2430 -2 2 2 4 40.92 35.95 2.2055 1 5 0 4 41.02 21.03 2.2002 0 2 2 4 41.47 2.98 2.1774 1 3 1 4 42.15 10.34 2.1438 0 6 0 2 42.19 10.21 2.1420 2 0 0 2 42.80 1.25 2.1129 2 1 0 4 43.30 44.65 2.0897 -2 3 2 4 44.07 16.85 2.0550 0 3 2 4 44.59 11.97 2.0323 2 2 0 4 45.65 1.10 1.9872 1 4 1 4 46.41 5.24 1.9565 -1 6 1 4 46.59 2.23 1.9493 0 6 1 4 47.42 2.02 1.9172 1 6 0 4 47.45 24.30 1.9162 2 3 0 4 47.70 7.15 1.9066 -1 5 2 4 49.03 1.41 1.8579 -2 0 3 2 49.58 3.34 1.8388 -2 1 3 4 50.11 3.96 1.8204 -2 5 1 4 50.63 2.92 1.8030 1 5 1 4 51.18 3.27 1.7849 -2 2 3 4 52.87 5.14 1.7316 0 5 2 4 52.93 1.56 1.7299 -3 0 2 2 53.41 1.31 1.7155 -1 7 1 4 53.56 22.42 1.7110 -1 6 2 4 53.57 1.33 1.7106 0 7 1 4 53.77 1.18 1.7047 -2 3 3 4 54.25 8.24 1.6909 1 0 2 2 54.27 3.03 1.6904 -1 3 3 4 54.32 9.97 1.6888 1 7 0 4 54.97 2.74 1.6705 -3 2 2 4 55.85 4.11 1.6461 2 5 0 4 56.15 2.46 1.6380 -3 1 1 4 56.25 2.06 1.6353 1 2 2 4 56.27 2.76 1.6349 1 6 1 4 56.95 4.32 1.6170 2 1 1 4 57.27 9.86 1.6087 -2 4 3 4 57.30 18.26 1.6079 0 8 0 2 57.44 9.36 1.6042 -3 3 2 4 57.73 3.58 1.5968 -2 6 2 4 57.74 4.96 1.5966 -1 4 3 4 57.79 9.23 1.5955 -3 0 3 2 58.36 20.79 1.5812 0 6 2 4 59.19 2.31 1.5610 0 0 3 2 59.67 1.26 1.5496 0 1 3 4 59.71 1.27 1.5485 -3 2 3 4 60.77 1.06 1.5242 -1 8 1 4 60.80 38.02 1.5235 -3 4 2 4 61.09 2.25 1.5170 0 2 3 4 61.16 29.79 1.5153 2 6 0 4 62.01 21.83 1.4966 1 4 2 4 62.03 3.21 1.4963 -1 5 3 4 63.41 5.05 1.4668 0 3 3 4 64.05 2.85 1.4538 2 4 1 4 64.96 3.00 1.4355 -3 5 2 4 65.77 15.36 1.4199 -2 0 4 2 65.80 1.19 1.4193 3 1 0 4 67.15 3.54 1.3941 3 2 0 4 67.56 2.11 1.3865 -2 2 4 4 68.83 5.92 1.3640 -2 8 1 4 69.26 4.20 1.3566 1 8 1 4 69.31 1.70 1.3558 1 9 0 4 70.57 13.06 1.3346 -2 8 2 4 70.57 1.83 1.3345 0 5 3 4 70.78 2.52 1.3311 -1 1 4 4 70.96 4.88 1.3281 -3 2 4 4 71.13 1.34 1.3255 0 8 2 4 72.33 1.36 1.3065 -2 7 3 4 73.13 2.44 1.2941 -3 3 4 4 73.67 1.43 1.2859 2 8 0 4 75.18 6.63 1.2638 2 0 2 2 75.60 2.62 1.2577 2 1 2 4 76.12 1.88 1.2506 -3 4 4 4 76.17 3.60 1.2498 1 1 3 4 77.21 12.56 1.2356 -1 4 4 4 77.48 1.46 1.2320 1 10 0 4 78.39 1.67 1.2199 0 9 2 4 78.43 1.29 1.2194 2 7 1 4 78.98 2.48 1.2122 2 3 2 4 80.88 2.49 1.1885 3 6 0 4 80.98 1.27 1.1873 -1 5 4 4 81.11 1.17 1.1857 3 1 1 4 81.90 1.71 1.1762 2 4 2 4 82.29 13.18 1.1717 -1 10 2 4 82.78 2.20 1.1659 0 1 4 4 84.03 1.06 1.1518 0 2 4 4 84.12 3.32 1.1508 -2 10 1 4 84.43 1.71 1.1473 3 3 1 4 84.52 1.21 1.1464 1 10 1 4 85.80 1.35 1.1325 -3 -8 3 4 86.09 2.79 1.1294 0 3 4 4 86.22 1.90 1.1281 1 11 0 4 86.99 1.85 1.1200 0 8 3 4 87.32 1.14 1.1166 3 4 1 4 88.71 2.43 1.1027 2 10 0 4 89.83 1.47 1.0918 -3 7 4 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.