LiGaSi2O6 Camara F, Nestola F, Angel R J, Ohashi H European Journal of Mineralogy 21 (2009) 599-614 Spontaneous strain variations through the low-temperature displacive phase transition of LiGaSi2O6 clinopyroxene Locality: synthetic Note: T = 150 K _database_code_amcsd 0007304 CELL PARAMETERS: 9.5134 8.5705 5.2372 90.000 109.910 90.000 SPACE GROUP: P2_1/c X-RAY WAVELENGTH: 1.541838 Cell Volume: 401.490 Density (g/cm3): 3.785 MAX. ABS. INTENSITY / VOLUME**2: 20.40069448 RIR: 1.755 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 14.31 82.17 6.1883 1 1 0 4 19.85 4.57 4.4724 2 0 0 2 20.23 46.11 4.3899 -1 1 1 4 20.73 30.85 4.2853 0 2 0 2 25.64 39.05 3.4749 1 1 1 4 30.28 100.00 2.9518 -2 2 1 4 31.46 1.00 2.8437 1 2 1 4 31.78 67.50 2.8160 3 1 0 4 32.91 8.42 2.7214 1 3 0 4 35.94 6.59 2.4988 -1 1 2 4 36.01 23.36 2.4937 -1 3 1 4 36.49 33.34 2.4621 0 0 2 2 37.81 30.89 2.3795 2 2 1 4 38.49 1.27 2.3387 -2 3 1 4 39.46 2.64 2.2838 1 3 1 4 40.15 3.70 2.2457 -3 1 2 4 41.12 2.20 2.1949 -2 2 2 4 41.21 1.92 2.1906 1 0 2 2 42.18 3.08 2.1426 0 4 0 2 42.60 18.84 2.1224 1 1 2 4 43.38 20.93 2.0858 -3 3 1 4 43.77 11.41 2.0680 -4 2 1 4 44.50 9.32 2.0360 -4 0 2 2 46.21 1.16 1.9647 0 4 1 4 47.03 2.01 1.9323 2 4 0 4 47.86 5.40 1.9007 2 0 2 2 47.98 14.15 1.8961 -2 4 1 4 49.06 8.00 1.8569 -5 1 1 4 49.57 3.40 1.8390 -4 2 2 4 50.59 2.93 1.8042 -3 3 2 4 51.94 1.86 1.7605 3 3 1 4 53.42 4.37 1.7150 2 4 1 4 54.34 1.23 1.6881 -1 1 3 4 54.51 8.28 1.6835 1 5 0 4 54.90 4.67 1.6724 4 2 1 4 56.98 9.11 1.6163 0 4 2 4 56.98 18.47 1.6162 -2 2 3 4 57.06 10.20 1.6141 3 1 2 4 58.14 2.50 1.5867 -4 4 1 4 58.28 18.26 1.5833 -5 3 1 4 59.78 8.41 1.5471 4 4 0 4 60.68 4.66 1.5261 -6 0 2 2 61.51 1.09 1.5075 -4 2 3 4 61.79 3.47 1.5013 1 1 3 4 61.87 2.75 1.4997 5 1 1 4 62.28 4.07 1.4908 6 0 0 2 62.35 1.41 1.4892 -2 3 3 4 62.50 6.57 1.4860 3 5 0 4 62.50 2.49 1.4860 -6 2 1 4 62.98 2.81 1.4759 -4 4 2 4 63.03 9.35 1.4747 -1 3 3 4 63.45 4.16 1.4660 -5 1 3 4 63.58 2.40 1.4633 -3 3 3 4 65.09 1.91 1.4331 -1 5 2 4 65.22 2.98 1.4305 4 0 2 2 65.33 7.39 1.4284 0 6 0 2 67.61 1.14 1.3856 4 4 1 4 67.92 7.54 1.3801 -3 5 2 4 69.24 1.87 1.3569 4 2 2 4 69.47 6.60 1.3531 -2 4 3 4 69.65 1.06 1.3499 1 5 2 4 69.77 1.91 1.3479 -2 6 1 4 69.93 3.30 1.3452 1 3 3 4 70.00 16.38 1.3441 5 3 1 4 71.07 3.48 1.3264 2 2 3 4 71.49 4.14 1.3197 -5 3 3 4 71.51 9.65 1.3193 -7 1 2 4 73.36 4.14 1.2906 -3 1 4 4 74.21 3.65 1.2778 -4 0 4 2 75.18 2.96 1.2639 7 1 0 4 76.05 1.91 1.2515 6 2 1 4 76.66 1.47 1.2430 -6 4 2 4 77.21 7.96 1.2355 0 6 2 4 77.55 2.03 1.2310 0 0 4 2 79.65 1.00 1.2038 4 6 0 4 80.70 1.90 1.1907 -1 7 1 4 80.78 1.12 1.1897 4 4 2 4 81.06 6.57 1.1863 3 5 2 4 82.49 1.27 1.1693 -4 6 2 4 82.83 2.71 1.1654 1 7 1 4 82.99 2.14 1.1635 -6 0 4 2 84.93 1.24 1.1419 2 6 2 4 85.27 1.12 1.1382 -8 -2 1 4 87.18 1.02 1.1181 8 0 0 2 89.25 1.13 1.0975 -4 4 4 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.