Nabalamprophyllite Sokolova E, Hawthorne F C The Canadian Mineralogist 46 (2008) 1323-1331 From structure topology to chemical composition. IV. Titanium silicates: The orthorhombic polytype of nabalamprophyllite from Lovozero Massif, Kola Peninsula, Russia Note: polytype nabalamprophyllite-2O Locality: Lovozero Massif, Kola Peninsula, Russia _database_code_amcsd 0019470 CELL PARAMETERS: 19.5640 7.1173 5.4144 90.000 90.000 90.000 SPACE GROUP: Pnmn X-RAY WAVELENGTH: 1.541838 Cell Volume: 753.917 Density (g/cm3): 3.515 MAX. ABS. INTENSITY / VOLUME**2: 10.56544540 RIR: 0.979 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 9.04 34.51 9.7820 2 0 0 2 13.24 5.27 6.6884 1 1 0 4 16.99 2.76 5.2182 1 0 1 4 18.45 2.54 4.8082 3 1 0 4 20.61 3.95 4.3092 0 1 1 4 21.11 2.23 4.2083 1 1 1 8 21.33 4.81 4.1657 3 0 1 4 22.55 40.10 3.9435 2 1 1 8 24.53 9.07 3.6294 4 0 1 4 24.76 71.13 3.5952 3 1 1 8 25.02 8.80 3.5587 0 2 0 2 25.99 36.17 3.4288 5 1 0 4 26.66 14.77 3.3442 2 2 0 4 27.35 56.51 3.2607 6 0 0 2 27.59 32.14 3.2333 4 1 1 8 28.14 7.01 3.1714 5 0 1 4 30.87 45.19 2.8968 5 1 1 8 31.08 21.81 2.8776 4 2 0 4 31.44 100.00 2.8453 2 2 1 8 32.04 15.70 2.7933 6 0 1 4 33.11 92.73 2.7058 3 2 1 8 33.41 50.44 2.6816 1 0 2 4 34.37 11.56 2.6091 2 0 2 4 34.48 29.85 2.6015 7 1 0 4 34.49 14.23 2.6002 6 1 1 8 35.32 3.42 2.5410 4 2 1 8 35.92 1.94 2.5003 3 0 2 4 36.17 8.07 2.4835 7 0 1 4 36.69 4.99 2.4497 2 1 2 8 37.41 3.89 2.4041 6 2 0 4 37.99 8.42 2.3686 4 0 2 4 38.00 7.74 2.3676 5 2 1 8 38.15 1.85 2.3590 3 1 2 8 38.39 2.66 2.3449 7 1 1 8 40.12 18.70 2.2474 4 1 2 8 40.46 4.71 2.2295 3 3 0 4 40.47 8.72 2.2287 8 0 1 4 40.52 1.22 2.2263 5 0 2 4 41.08 4.43 2.1972 6 2 1 8 41.83 7.22 2.1597 1 3 1 8 41.93 1.61 2.1546 0 2 2 4 42.20 44.02 2.1417 1 2 2 8 42.62 6.29 2.1213 2 3 1 8 42.98 1.67 2.1042 2 2 2 8 43.45 7.11 2.0829 6 0 2 4 43.53 16.61 2.0790 9 1 0 4 43.92 3.31 2.0616 3 3 1 8 44.27 15.89 2.0458 3 2 2 8 44.49 15.80 2.0366 7 2 1 8 44.67 24.41 2.0287 5 3 0 4 44.94 2.91 2.0173 9 0 1 4 45.37 25.41 1.9990 6 1 2 8 45.69 1.52 1.9858 4 3 1 8 46.41 1.10 1.9564 10 0 0 2 46.81 5.71 1.9408 9 1 1 8 47.88 9.07 1.8997 5 3 1 8 48.53 3.60 1.8758 7 1 2 8 49.54 2.11 1.8400 10 0 1 4 50.28 3.39 1.8147 8 0 2 4 50.46 10.62 1.8087 7 3 0 4 50.47 4.75 1.8082 6 3 1 8 51.29 5.43 1.7814 10 1 1 8 51.35 28.49 1.7793 0 4 0 2 52.00 10.38 1.7585 8 1 2 8 52.11 11.93 1.7553 2 3 2 8 52.12 3.30 1.7549 9 2 1 8 53.08 1.08 1.7255 11 1 0 4 53.19 2.82 1.7221 2 1 3 8 53.45 1.62 1.7144 10 2 0 4 53.72 3.52 1.7064 7 2 2 8 54.11 3.12 1.6950 9 0 2 4 54.29 3.00 1.6897 3 1 3 8 54.91 1.02 1.6721 4 4 0 4 55.14 1.12 1.6657 2 4 1 8 55.81 13.43 1.6472 4 1 3 8 55.93 8.24 1.6440 11 1 1 8 56.12 3.02 1.6389 5 0 3 4 56.22 1.00 1.6363 3 4 1 8 56.29 5.72 1.6344 10 2 1 8 57.44 26.79 1.6042 1 2 3 8 57.50 2.56 1.6027 9 3 0 4 57.70 1.28 1.5977 4 4 1 8 57.72 1.00 1.5971 5 1 3 8 58.08 3.00 1.5883 2 2 3 8 58.18 3.60 1.5857 10 0 2 4 59.01 10.58 1.5652 6 3 2 8 59.12 1.05 1.5627 3 2 3 8 59.15 3.02 1.5619 6 4 0 4 59.58 1.36 1.5518 5 4 1 8 59.75 1.37 1.5477 10 1 2 8 60.01 2.86 1.5416 6 1 3 8 60.50 2.55 1.5303 9 2 2 8 60.67 23.80 1.5264 11 2 1 8 60.74 2.95 1.5248 12 1 1 8 61.12 2.89 1.5162 7 0 3 4 61.68 1.53 1.5039 7 3 2 8 61.82 3.85 1.5007 6 4 1 8 62.38 6.21 1.4886 5 2 3 8 62.66 20.87 1.4826 1 4 2 8 62.68 1.44 1.4822 12 2 0 4 63.26 3.90 1.4700 2 4 2 8 64.42 2.22 1.4464 7 4 1 8 64.67 20.06 1.4414 8 3 2 8 64.92 2.58 1.4364 0 3 3 4 65.27 14.92 1.4296 12 2 1 8 65.60 1.37 1.4231 11 3 0 4 65.63 2.38 1.4226 4 4 2 8 65.72 1.04 1.4208 13 1 1 8 66.96 6.43 1.3974 14 0 0 2 67.01 2.38 1.3966 12 0 2 4 67.34 2.20 1.3905 8 4 1 8 67.45 1.67 1.3886 9 0 3 4 68.02 3.50 1.3782 4 3 3 8 68.13 1.90 1.3763 11 3 1 8 68.87 1.04 1.3632 2 5 1 8 69.44 5.10 1.3536 0 0 4 2 69.48 1.55 1.3529 6 4 2 8 69.63 2.95 1.3504 1 0 4 4 69.83 5.30 1.3470 3 5 1 8 70.19 6.45 1.3408 2 0 4 4 71.15 3.85 1.3252 4 5 1 8 71.57 4.19 1.3183 10 3 2 8 71.76 11.62 1.3153 13 0 2 4 72.45 2.74 1.3046 4 0 4 4 72.48 3.00 1.3041 12 3 1 8 72.48 5.13 1.3041 10 1 3 8 72.69 1.90 1.3007 14 2 0 4 72.83 4.15 1.2986 5 5 1 8 73.16 2.87 1.2936 9 2 3 8 74.13 1.08 1.2791 10 4 1 8 74.71 1.59 1.2705 8 4 2 8 74.86 1.42 1.2684 7 5 0 4 74.87 1.09 1.2683 6 5 1 8 75.51 1.06 1.2590 5 1 4 8 75.82 1.81 1.2547 2 2 4 8 76.19 3.74 1.2496 2 5 2 8 76.36 1.03 1.2472 11 1 3 8 77.09 3.22 1.2372 13 3 1 8 77.53 1.00 1.2313 6 1 4 8 78.01 1.59 1.2249 4 2 4 8 78.37 2.99 1.2201 4 5 2 8 79.51 1.51 1.2055 5 4 3 8 79.88 4.11 1.2008 7 1 4 8 80.48 3.77 1.1934 11 2 3 8 80.54 1.55 1.1927 12 1 3 8 80.69 2.48 1.1909 9 5 0 4 81.07 2.71 1.1862 0 6 0 2 81.27 1.66 1.1838 10 4 2 8 81.79 1.38 1.1776 2 6 0 4 81.99 2.57 1.1752 6 5 2 8 82.01 3.96 1.1750 15 0 2 4 83.03 2.16 1.1631 9 5 1 8 83.62 1.77 1.1564 16 2 0 4 83.83 1.93 1.1540 7 4 3 8 84.13 1.69 1.1507 2 6 1 8 84.60 1.47 1.1454 12 2 3 8 84.83 1.24 1.1429 15 3 0 4 85.02 3.32 1.1409 3 6 1 8 85.63 2.24 1.1344 9 1 4 8 85.95 1.90 1.1309 16 2 1 8 86.42 3.45 1.1260 5 3 4 8 86.43 2.59 1.1259 10 5 1 8 87.41 1.35 1.1158 15 2 2 8 87.67 2.24 1.1131 10 0 4 4 87.79 1.09 1.1119 17 1 1 8 87.84 1.33 1.1113 11 5 0 4 88.38 1.08 1.1060 6 3 4 8 89.06 5.53 1.0993 13 2 3 8 89.09 6.12 1.0990 14 4 0 4 89.13 1.26 1.0986 12 4 2 8 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.