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 #BN82, P = 0 GPa Locality: synthetic _database_code_amcsd 0018953 CELL PARAMETERS: 5.8490 8.7900 13.1320 90.000 90.000 90.000 SPACE GROUP: Cmcm X-RAY WAVELENGTH: 1.541838 Cell Volume: 675.152 Density (g/cm3): 3.092 MAX. ABS. INTENSITY / VOLUME**2: 6.681507911 RIR: 0.703 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 13.49 39.03 6.5660 0 0 2 2 18.22 46.65 4.8695 1 1 0 4 19.44 20.00 4.5657 1 1 1 8 21.32 23.82 4.1678 0 2 1 4 22.74 11.42 3.9113 1 1 2 8 24.37 59.83 3.6523 0 2 2 4 27.16 3.79 3.2830 0 0 4 2 27.40 19.13 3.2554 1 1 3 8 30.57 26.74 2.9245 2 0 0 2 32.90 100.00 2.7221 1 1 4 8 33.55 44.34 2.6715 2 0 2 4 34.09 67.20 2.6302 0 2 4 4 34.23 51.28 2.6197 1 3 0 4 34.92 6.23 2.5691 1 3 1 8 36.92 32.23 2.4347 2 2 0 4 36.94 28.67 2.4332 1 3 2 8 37.57 15.89 2.3939 2 2 1 8 38.96 7.75 2.3116 1 1 5 8 39.47 10.10 2.2828 2 2 2 8 39.99 22.66 2.2545 0 2 5 4 40.11 1.72 2.2479 1 3 3 8 41.07 2.48 2.1975 0 4 0 2 41.25 7.54 2.1887 0 0 6 2 41.35 3.87 2.1837 2 0 4 4 41.67 2.44 2.1674 0 4 1 4 42.49 48.32 2.1277 2 2 3 8 43.42 3.14 2.0839 0 4 2 4 45.43 1.08 1.9963 1 1 6 8 46.23 21.41 1.9639 0 4 3 4 46.34 4.32 1.9592 0 2 6 4 48.32 4.62 1.8837 3 1 1 8 51.16 3.14 1.7855 2 2 5 8 52.06 1.17 1.7568 2 4 0 4 52.20 20.44 1.7523 2 0 6 4 52.26 1.23 1.7506 1 1 7 8 52.56 4.01 1.7413 2 4 1 8 53.08 13.81 1.7254 0 2 7 4 54.03 6.61 1.6971 2 4 2 8 54.44 2.89 1.6854 0 4 5 4 54.50 4.65 1.6836 1 5 0 4 54.64 3.04 1.6796 1 3 6 8 54.99 3.18 1.6699 1 5 1 8 55.83 9.28 1.6467 3 1 4 8 56.02 17.33 1.6415 0 0 8 2 56.44 14.32 1.6304 2 4 3 8 56.54 8.69 1.6277 2 2 6 8 56.71 14.73 1.6232 3 3 0 4 58.58 4.66 1.5757 3 3 2 8 59.42 2.46 1.5555 1 1 8 8 59.62 13.84 1.5507 0 4 6 4 59.70 65.81 1.5490 2 4 4 8 61.94 1.88 1.4981 1 5 4 8 63.63 24.74 1.4622 4 0 0 2 63.73 2.46 1.4602 2 4 5 8 65.25 1.68 1.4298 0 6 2 4 65.41 1.28 1.4268 0 4 7 4 67.31 13.66 1.3910 1 3 8 8 69.00 14.53 1.3611 2 2 8 8 69.21 4.04 1.3575 4 2 2 8 70.37 2.35 1.3378 0 6 4 4 70.48 1.62 1.3361 3 1 7 8 71.78 2.59 1.3151 0 4 8 4 72.11 12.08 1.3098 2 6 0 4 72.38 3.52 1.3056 3 5 0 4 72.50 1.57 1.3038 3 3 6 8 72.52 2.68 1.3034 2 6 1 8 72.79 2.10 1.2992 3 5 1 8 73.76 2.93 1.2845 2 6 2 8 73.91 2.64 1.2823 2 4 7 8 74.20 11.49 1.2780 4 2 4 8 75.81 5.74 1.2549 2 6 3 8 75.94 1.17 1.2530 1 5 7 8 77.86 2.19 1.2268 4 2 5 8 78.20 1.08 1.2224 1 7 1 8 78.58 2.17 1.2174 0 6 6 4 78.91 2.73 1.2132 3 5 4 8 80.11 11.68 1.1980 2 0 10 4 80.19 1.41 1.1970 4 4 2 8 81.41 2.09 1.1821 1 7 3 8 81.98 1.12 1.1753 1 5 8 8 82.09 1.75 1.1740 1 3 10 8 82.19 4.28 1.1729 4 4 3 8 82.27 1.27 1.1718 4 2 6 8 83.34 1.09 1.1596 5 1 0 4 83.35 1.10 1.1595 1 1 11 8 83.67 1.97 1.1558 2 2 10 8 83.82 8.46 1.1542 3 3 8 8 84.00 1.02 1.1521 0 2 11 4 84.19 3.36 1.1500 1 7 4 8 86.30 1.80 1.1273 0 4 10 4 87.43 2.90 1.1155 4 2 7 8 87.76 4.09 1.1122 1 7 5 8 88.53 1.03 1.1045 4 4 5 8 89.12 2.56 1.0987 0 8 0 2 89.67 5.42 1.0934 5 1 4 8 89.83 6.45 1.0919 4 0 8 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.