Sekaninaite Hochella M F, Brown G E, Ross F K, Gibbs G V American Mineralogist 64 (1979) 337-351 High-temperature crystal chemistry of hydrous Mg- and Fe-cordierite Dolni Bory, T = 24 C _database_code_amcsd 0000709 CELL PARAMETERS: 17.2300 9.8350 9.3140 90.000 90.000 90.000 SPACE GROUP: Cccm X-RAY WAVELENGTH: 1.541838 Cell Volume: 1578.323 Density (g/cm3): 2.682 MAX. ABS. INTENSITY / VOLUME**2: 16.20201904 RIR: 1.967 RIR based on corundum from Acta Crystallographica A38 (1982) 733-739 2-THETA INTENSITY D-SPACING H K L Multiplicity 10.27 56.04 8.6150 2 0 0 2 10.36 100.00 8.5415 1 1 0 4 17.88 2.51 4.9596 3 1 0 4 19.06 1.13 4.6570 0 0 2 2 21.69 10.72 4.0967 2 0 2 4 21.74 48.40 4.0888 1 1 2 8 26.25 46.73 3.3949 3 1 2 8 26.36 27.08 3.3813 0 2 2 4 27.70 1.30 3.2206 1 3 0 4 28.22 7.25 3.1622 4 0 2 4 28.35 22.41 3.1476 2 2 2 8 29.08 20.95 3.0704 5 1 1 8 29.18 17.35 3.0603 4 2 1 8 29.34 20.81 3.0437 1 3 1 8 31.14 2.31 2.8717 6 0 0 2 31.42 2.72 2.8472 3 3 0 4 33.61 9.66 2.6663 5 1 2 8 33.70 10.84 2.6597 4 2 2 8 33.84 6.08 2.6489 1 3 2 8 36.22 6.17 2.4798 6 2 0 4 36.55 3.86 2.4588 0 4 0 2 38.67 10.62 2.3285 0 0 4 2 41.24 7.41 2.1888 6 2 2 8 41.53 2.92 2.1743 0 4 2 4 42.55 3.83 2.1248 7 1 2 8 42.73 3.92 2.1159 5 3 2 8 42.90 5.42 2.1082 2 4 2 8 44.22 1.25 2.0484 4 0 4 4 44.31 1.96 2.0444 2 2 4 8 46.00 1.38 1.9728 8 2 0 4 46.11 2.77 1.9684 7 3 0 4 46.47 1.53 1.9543 1 5 0 4 47.09 1.06 1.9300 8 2 1 8 48.07 2.29 1.8927 7 1 3 8 48.12 1.50 1.8909 4 2 4 8 48.23 2.15 1.8870 1 3 4 8 48.24 3.39 1.8865 5 3 3 8 48.39 3.34 1.8810 2 4 3 8 48.44 2.92 1.8792 9 1 0 4 48.76 2.91 1.8677 6 4 0 4 48.95 3.19 1.8609 3 5 0 4 49.79 1.62 1.8312 6 4 1 8 49.98 1.12 1.8248 3 5 1 8 50.46 3.24 1.8086 6 0 4 4 50.64 6.37 1.8025 3 3 4 8 52.51 2.11 1.7426 9 1 2 8 52.81 2.22 1.7335 6 4 2 8 52.99 1.90 1.7280 3 5 2 8 53.16 3.69 1.7230 10 0 0 2 53.65 4.39 1.7083 5 5 0 4 54.02 14.78 1.6975 6 2 4 8 54.26 7.93 1.6907 0 4 4 4 55.09 1.68 1.6671 7 1 4 8 57.31 1.92 1.6076 9 1 3 8 57.59 3.07 1.6004 6 4 3 8 57.76 1.89 1.5961 3 5 3 8 59.32 2.47 1.5579 9 3 2 8 59.81 1.69 1.5462 0 6 2 4 60.29 1.25 1.5352 10 2 2 8 61.62 2.12 1.5052 8 2 4 8 61.71 3.13 1.5032 7 3 4 8 61.99 2.07 1.4969 1 5 4 8 62.72 3.27 1.4815 3 1 6 8 62.77 1.55 1.4803 0 2 6 4 63.36 1.37 1.4680 11 1 2 8 63.78 3.56 1.4592 7 5 2 8 63.98 1.80 1.4553 4 6 2 8 65.58 1.68 1.4236 6 6 0 4 66.77 1.44 1.4009 5 1 6 8 66.83 1.85 1.4000 4 2 6 8 66.91 1.19 1.3984 1 3 6 8 68.02 1.19 1.3783 12 2 0 4 68.37 4.36 1.3721 12 0 2 4 68.38 1.08 1.3719 9 5 0 4 68.79 1.31 1.3648 3 7 0 4 68.86 1.08 1.3634 12 2 1 8 68.98 7.26 1.3614 6 6 2 8 69.22 1.23 1.3573 9 5 1 8 69.63 1.25 1.3503 3 7 1 8 70.66 1.53 1.3332 10 2 4 8 70.86 1.20 1.3299 8 4 4 8 71.73 2.77 1.3158 6 2 6 8 71.93 1.16 1.3126 0 4 6 4 72.65 1.09 1.3015 7 1 6 8 73.64 1.60 1.2863 11 3 3 8 74.30 1.21 1.2765 1 7 3 8 77.51 1.38 1.2315 5 1 7 8 77.56 1.08 1.2308 4 2 7 8 77.64 1.30 1.2297 1 3 7 8 79.41 2.42 1.2068 10 4 4 8 79.94 1.22 1.2001 1 7 4 8 80.09 3.03 1.1982 12 4 2 8 80.87 1.46 1.1887 0 8 2 4 81.08 2.11 1.1861 12 2 4 8 81.42 1.46 1.1820 9 5 4 8 81.80 2.02 1.1774 3 7 4 8 82.93 2.81 1.1643 0 0 8 2 85.88 1.15 1.1316 9 3 6 8 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.