Tremolite Warren B Zeitschrift fur Kristallographie 72 (1929) 42-57 The structure of tremolite H2 Ca2 Mg5 (Si O3)8 _cod_database_code 1011222 _database_code_amcsd 0018086 CELL PARAMETERS: 9.7700 17.8000 5.2600 90.000 73.970 90.000 SPACE GROUP: I2/m X-RAY WAVELENGTH: 1.541838 Cell Volume: 879.177 Density (g/cm3): 3.061 MAX. ABS. INTENSITY / VOLUME**2: 6.726651982 RIR: 0.716 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 9.94 48.67 8.9000 0 2 0 2 10.65 16.09 8.3053 1 1 0 4 17.48 7.36 5.0745 1 0 1 2 17.68 15.14 5.0159 1 3 0 4 18.24 39.98 4.8631 0 1 1 4 18.90 9.97 4.6951 2 0 0 2 19.95 8.28 4.4500 0 4 0 2 21.40 5.51 4.1527 2 2 0 4 22.15 4.00 4.0128 -1 0 1 2 22.56 2.88 3.9412 2 1 1 4 23.11 28.01 3.8481 0 3 1 4 26.69 51.82 3.3402 2 3 1 4 27.62 13.19 3.2298 2 4 0 4 28.96 39.98 3.0827 3 1 0 4 29.11 1.88 3.0672 3 0 1 2 29.98 1.26 2.9801 -1 4 1 4 30.72 10.49 2.9107 0 5 1 4 30.83 36.69 2.8998 3 2 1 4 32.34 6.11 2.7684 3 3 0 4 33.05 21.97 2.7100 -2 3 1 4 33.55 100.00 2.6714 2 5 1 4 35.04 46.71 2.5611 1 6 1 4 35.38 14.41 2.5372 2 0 2 2 35.51 47.86 2.5277 0 0 2 2 36.97 2.75 2.4316 0 2 2 4 37.71 4.68 2.3855 -1 6 1 4 38.29 8.58 2.3507 3 5 0 4 38.91 54.17 2.3146 -2 5 1 4 39.13 14.03 2.3019 -3 2 1 4 39.48 1.38 2.2826 3 1 2 4 39.68 9.30 2.2717 0 7 1 4 39.71 1.42 2.2699 4 2 0 4 39.73 16.99 2.2688 -1 1 2 4 40.54 1.11 2.2250 0 8 0 2 40.59 1.05 2.2225 4 3 1 4 41.07 4.43 2.1979 0 4 2 4 41.98 1.97 2.1523 2 7 1 4 42.35 2.49 2.1343 -1 3 2 4 42.39 28.01 2.1324 3 6 1 4 42.75 4.21 2.1153 1 5 2 4 44.85 29.31 2.0207 4 0 2 2 45.09 4.74 2.0106 2 8 0 4 45.19 8.00 2.0064 -2 0 2 2 45.63 6.30 1.9883 4 5 1 4 45.98 4.10 1.9736 3 7 0 4 46.06 1.01 1.9706 4 2 2 4 46.52 4.10 1.9521 -2 7 1 4 46.95 4.45 1.9353 1 9 0 4 47.23 2.89 1.9244 -1 5 2 4 47.89 1.41 1.8996 5 2 1 4 49.03 1.84 1.8578 -3 6 1 4 49.49 3.37 1.8418 0 9 1 4 49.54 2.12 1.8399 4 4 2 4 49.86 4.59 1.8291 -2 4 2 4 49.89 8.78 1.8281 1 7 2 4 51.01 2.10 1.7905 5 3 0 4 51.33 3.33 1.7800 0 10 0 2 52.70 2.30 1.7367 -3 1 2 4 53.91 1.29 1.7006 -1 7 2 4 53.94 2.91 1.7000 -4 5 1 4 54.45 1.49 1.6853 5 3 2 4 54.64 2.81 1.6797 1 10 1 4 54.78 8.10 1.6757 2 3 3 4 54.88 2.58 1.6729 2 8 2 4 54.98 11.23 1.6701 0 8 2 4 55.28 4.87 1.6618 3 2 3 4 56.56 1.25 1.6271 -1 10 1 4 56.59 8.92 1.6263 5 6 1 4 57.03 5.91 1.6149 4 8 0 4 57.82 6.03 1.5947 1 11 0 4 58.89 22.26 1.5682 2 5 3 4 59.02 8.09 1.5650 6 0 0 2 60.03 1.15 1.5412 0 11 1 4 60.36 7.71 1.5336 6 0 2 2 60.81 5.63 1.5231 -4 0 2 2 61.37 5.63 1.5107 5 7 0 4 61.68 16.74 1.5038 1 6 3 4 61.85 3.11 1.5000 3 9 2 4 62.31 3.88 1.4900 -2 8 2 4 62.63 7.58 1.4833 0 12 0 2 62.78 1.32 1.4800 6 5 1 4 63.97 2.30 1.4554 0 10 2 4 64.10 2.18 1.4528 5 2 3 4 64.24 1.83 1.4499 6 4 2 4 64.44 1.76 1.4459 5 7 2 4 64.68 2.14 1.4411 -4 4 2 4 64.74 2.55 1.4398 2 7 3 4 64.87 3.84 1.4374 3 11 0 4 65.65 28.19 1.4221 -5 6 1 4 66.06 1.02 1.4144 2 12 0 4 67.99 1.65 1.3788 7 2 1 4 69.47 3.96 1.3531 -2 5 3 4 69.92 7.19 1.3453 7 1 2 4 70.38 3.48 1.3377 7 1 0 4 70.43 1.48 1.3369 -5 1 2 4 71.24 5.95 1.3238 3 11 2 4 71.37 5.78 1.3216 0 13 1 4 71.40 2.64 1.3210 -1 11 2 4 71.53 3.69 1.3190 5 6 3 4 71.74 2.05 1.3156 7 3 2 4 72.19 2.25 1.3085 -3 9 2 4 72.25 1.79 1.3077 -5 3 2 4 72.74 5.32 1.3001 3 1 4 4 72.95 2.62 1.2968 2 13 1 4 73.06 1.60 1.2952 -6 5 1 4 74.03 3.53 1.2806 2 12 2 4 74.11 6.72 1.2793 0 12 2 4 74.53 1.43 1.2732 3 3 4 4 74.70 1.13 1.2708 1 3 4 4 74.84 3.70 1.2686 4 0 4 2 75.17 3.78 1.2639 0 0 4 2 75.24 2.92 1.2629 7 6 1 4 78.68 1.54 1.2161 7 2 3 4 78.71 1.62 1.2158 0 4 4 4 79.00 1.69 1.2120 -1 14 1 4 79.56 1.10 1.2048 -7 2 1 4 81.04 4.86 1.1865 -3 11 2 4 81.09 2.01 1.1859 -5 7 2 4 81.30 1.05 1.1835 -1 10 3 4 82.11 1.69 1.1738 8 0 0 2 83.82 1.87 1.1541 8 5 1 4 84.12 1.70 1.1508 6 0 4 2 85.60 1.59 1.1346 5 10 3 4 86.50 1.40 1.1252 -7 6 1 4 87.96 2.42 1.1102 7 9 0 4 89.04 1.09 1.0995 8 3 3 4 89.33 1.05 1.0966 5 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.