Kenotobermorite Merlino S, Bonaccorsi E, Armbruster T European Journal of Mineralogy 13 (2001) 577-590 The real structure of tobermorite 11A: normal and anomalous forms, OD character and polytypic modifications Note: MDO2 - synchrotron radiation source, polytype kenotobermorite-2M Locality: Bascenov, Urals, Russia _database_code_amcsd 0006887 CELL PARAMETERS: 6.7320 7.3690 22.6800 90.000 90.000 123.180 SPACE GROUP: Bm X-RAY WAVELENGTH: 1.541838 Cell Volume: 941.668 Density (g/cm3): 2.545 MAX. ABS. INTENSITY / VOLUME**2: 10.57564207 RIR: 1.353 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 7.80 100.00 11.3400 0 0 2 2 14.36 2.07 6.1675 0 1 0 1 14.89 4.95 5.9512 1 -1 1 2 15.63 2.03 5.6700 0 0 4 2 16.21 18.39 5.4682 1 0 1 2 16.36 6.51 5.4180 0 1 2 2 18.57 3.68 4.7788 1 -1 3 2 23.54 1.89 3.7800 0 0 6 2 24.36 4.34 3.6541 1 -1 5 2 24.48 4.70 3.6368 -1 2 1 2 25.21 21.45 3.5333 1 0 5 2 26.64 3.37 3.3465 -2 1 0 1 26.92 5.17 3.3121 -1 2 3 2 26.93 4.48 3.3108 1 1 1 2 27.68 10.23 3.2229 0 1 6 2 27.80 3.53 3.2097 2 -1 2 2 28.95 25.82 3.0838 0 2 0 1 28.96 26.94 3.0836 -2 2 0 1 29.18 3.94 3.0602 1 1 3 2 30.03 28.54 2.9757 0 2 2 2 30.03 28.32 2.9756 2 -2 2 2 31.03 1.72 2.8820 2 -1 4 2 31.18 6.73 2.8683 1 -1 7 2 31.28 2.39 2.8599 -1 2 5 2 31.56 9.19 2.8350 0 0 8 2 31.76 15.17 2.8172 2 0 0 1 31.86 26.75 2.8087 1 0 7 2 32.76 7.20 2.7341 2 0 2 2 33.07 1.58 2.7090 0 2 4 2 33.07 1.59 2.7089 2 -2 4 2 33.27 1.25 2.6930 1 1 5 2 34.83 1.90 2.5759 0 1 8 2 35.58 11.46 2.5229 2 0 4 2 35.84 2.59 2.5056 2 -1 6 2 36.94 8.74 2.4331 -1 2 7 2 38.68 1.82 2.3278 1 1 7 2 39.16 9.44 2.3004 1 0 9 2 39.74 9.61 2.2680 0 0 10 2 42.11 5.35 2.1460 1 2 3 2 42.11 4.94 2.1459 3 -2 3 2 42.47 1.20 2.1286 0 1 10 2 43.35 3.26 2.0871 0 2 8 2 43.36 3.19 2.0870 2 -2 8 2 43.51 5.20 2.0800 -1 2 9 2 44.05 1.04 2.0558 0 3 0 1 44.24 1.20 2.0474 3 -3 1 2 45.18 7.05 2.0070 1 2 5 2 45.18 7.22 2.0069 3 -2 5 2 46.44 1.05 1.9554 1 -1 11 2 48.63 1.15 1.8724 3 -3 5 2 49.48 14.94 1.8422 -2 4 0 1 49.50 7.63 1.8414 1 2 7 2 49.50 7.70 1.8414 3 -2 7 2 49.91 2.79 1.8271 0 2 10 2 49.92 2.84 1.8270 2 -2 10 2 50.17 1.83 1.8184 -2 4 2 2 50.54 2.10 1.8060 0 3 6 2 52.67 1.43 1.7379 -1 3 9 2 52.75 2.39 1.7353 3 0 5 2 54.86 4.26 1.6734 1 2 9 2 54.87 4.24 1.6733 3 -2 9 2 54.87 5.11 1.6733 2 2 0 1 54.87 5.26 1.6732 -4 2 0 1 55.11 3.17 1.6666 1 0 13 2 56.65 6.50 1.6249 3 0 7 2 56.83 1.01 1.6200 0 0 14 2 59.88 1.71 1.5447 -2 4 8 2 60.06 2.56 1.5405 -1 4 7 2 60.06 2.52 1.5404 -3 4 7 2 60.81 1.00 1.5232 0 3 10 2 61.59 1.13 1.5059 3 0 9 2 64.84 1.24 1.4380 -1 4 9 2 64.84 1.34 1.4380 -3 4 9 2 65.25 1.43 1.4300 -2 4 10 2 66.36 2.60 1.4086 4 0 0 1 66.89 1.31 1.3988 -1 2 15 2 66.94 2.39 1.3979 4 0 2 2 68.15 2.16 1.3759 1 2 13 2 68.15 2.18 1.3759 3 -2 13 2 68.89 1.07 1.3630 -2 5 6 2 73.53 1.43 1.2879 0 2 16 2 73.53 1.47 1.2879 2 -2 16 2 75.01 1.49 1.2662 2 0 16 2 75.95 1.56 1.2529 1 2 15 2 75.95 1.60 1.2529 3 -2 15 2 78.49 1.54 1.2186 1 4 7 2 78.49 1.57 1.2186 5 -4 7 2 81.77 1.25 1.1778 3 0 15 2 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.