Ferroericssonite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from single crystal data of R070406 Kampf A R, Roberts A C, Venance K E, Dunning G E, Walstrom R E The Canadian Mineralogist 49 (2011) 587-594 Ferroericssonite, the Fe2+ analogue of ericssonite, from eastern Fresno County, California, U.S.A. Locality: Esquire #8 claim, Big Creek, eastern Fresno County, California, USA _database_code_amcsd 0018382 CELL PARAMETERS: 20.3020 6.9991 5.3751 90.000 94.835 90.000 SPACE GROUP: C2/m ATOM X Y Z OCCUPANCY ISO(B) Ba 0.22505 0.00000 0.24144 1.000 0.755 Fe 0.00000 0.26153 0.00000 1.000 0.955 Fe 0.00000 0.00000 0.50000 1.000 0.979 Fe 0.00000 0.50000 0.50000 1.000 0.845 Fe 0.14026 0.50000 0.21580 1.000 0.537 Si 0.13431 0.22566 0.71250 1.000 0.490 OH 0.05550 0.00000 0.18020 0.770 3.000 Cl 0.05550 0.00000 0.18020 0.230 3.000 O 0.15740 0.00000 0.71950 1.000 0.995 O 0.05466 0.24550 0.68460 1.000 0.782 O 0.16858 0.30900 0.97320 1.000 0.829 O 0.16897 0.30920 0.47610 1.000 0.829 O 0.04970 0.50000 0.19220 1.000 0.797 X-RAY WAVELENGTH: 1.541838 BOUNDS ON TWO THETA: 5.0 90.0 LIMITS IMPOSED ON THE INDICES ARE: +/- 18 +/- 6 +/- 4 MAX. ABS. INTENSITY / VOLUME**2: 23.76932708 The INTENSITY cut off value is 1.00 2-THETA INTENSITY D-SPACING H K L 13.39 2.22 6.6144 1 1 0 17.54 19.01 5.0574 4 0 0 19.40 1.81 4.5765 2 0 1 21.05 9.73 4.2197 -1 1 1 21.64 20.27 4.1075 1 1 1 23.15 5.09 3.8424 -4 0 1 23.98 54.14 3.7114 -3 1 1 25.22 7.59 3.5316 4 0 1 25.43 18.08 3.5028 5 1 0 25.45 12.63 3.4996 0 2 0 25.50 59.65 3.4936 3 1 1 26.44 23.92 3.3716 6 0 0 26.96 22.50 3.3072 2 2 0 29.43 50.47 3.0347 -5 1 1 30.11 9.94 2.9684 -6 0 1 30.51 5.17 2.9296 0 2 1 31.08 19.65 2.8778 4 2 0 31.40 7.09 2.8493 -2 2 1 31.52 38.35 2.8382 5 1 1 32.20 100.00 2.7799 2 2 1 32.55 9.32 2.7507 6 0 1 33.46 7.91 2.6780 0 0 2 33.55 34.38 2.6712 7 1 0 33.90 39.10 2.6445 -2 0 2 34.67 27.75 2.5873 -4 2 1 35.39 6.94 2.5364 2 0 2 35.50 10.84 2.5287 8 0 0 36.13 7.09 2.4858 4 2 1 36.40 7.45 2.4685 -7 1 1 36.62 6.47 2.4537 -4 0 2 37.02 7.61 2.4281 6 2 0 38.05 5.85 2.3649 -8 0 1 39.40 3.30 2.2871 3 1 2 39.82 2.14 2.2637 -6 2 1 40.72 4.76 2.2157 8 0 1 40.90 6.35 2.2066 -5 1 2 40.93 1.46 2.2048 3 3 0 41.25 14.42 2.1888 -6 0 2 41.77 21.03 2.1626 6 2 1 42.23 10.81 2.1401 9 1 0 42.34 6.00 2.1346 -1 3 1 42.51 21.24 2.1267 0 2 2 42.66 3.66 2.1196 1 3 1 42.86 17.31 2.1099 -2 2 2 43.98 6.04 2.0589 -3 3 1 44.04 10.45 2.0563 5 1 2 44.09 9.07 2.0537 2 2 2 44.19 1.86 2.0496 8 2 0 44.30 1.37 2.0447 -9 1 1 44.85 13.07 2.0211 5 3 0 44.89 10.47 2.0193 3 3 1 44.97 9.88 2.0159 6 0 2 45.13 4.92 2.0091 -4 2 2 46.09 9.20 1.9695 -7 1 2 46.34 11.62 1.9595 -8 2 1 46.64 3.35 1.9475 -10 0 1 46.97 1.51 1.9346 9 1 1 47.40 10.18 1.9178 -5 3 1 48.64 1.40 1.8720 8 2 1 48.83 5.85 1.8652 5 3 1 49.49 2.91 1.8419 10 0 1 50.07 6.19 1.8216 7 1 2 50.26 8.00 1.8153 7 3 0 51.37 3.08 1.7787 11 1 0 52.28 26.21 1.7498 0 4 0 52.35 1.70 1.7476 -7 3 1 52.46 1.92 1.7442 1 3 2 52.55 4.68 1.7414 -9 1 2 53.53 2.60 1.7118 1 1 3 53.61 3.18 1.7096 -3 1 3 54.20 1.13 1.6922 7 3 1 54.49 9.07 1.6839 -10 0 2 55.58 3.28 1.6536 4 4 0 55.77 1.99 1.6483 -12 0 1 55.94 7.73 1.6437 3 1 3 56.05 1.23 1.6407 4 0 3 56.09 7.31 1.6398 -5 1 3 56.23 1.17 1.6358 -6 0 3 56.46 27.56 1.6299 10 2 1 56.88 1.41 1.6187 9 3 0 57.22 1.79 1.6100 9 1 2 57.91 1.10 1.5924 -4 4 1 57.99 12.50 1.5903 0 2 3 58.03 12.94 1.5894 -2 2 3 58.35 3.65 1.5815 5 3 2 58.79 1.66 1.5706 12 0 1 58.90 1.32 1.5679 4 4 1 59.55 2.30 1.5525 10 0 2 59.84 2.79 1.5457 5 1 3 60.04 7.28 1.5410 -7 3 2 60.04 2.87 1.5408 -7 1 3 60.71 1.34 1.5255 6 0 3 60.95 1.27 1.5201 -8 0 3 61.00 1.69 1.5190 13 1 0 61.52 1.78 1.5074 -6 4 1 62.26 23.65 1.4912 -12 2 1 62.52 3.71 1.4855 4 2 3 62.59 2.72 1.4842 -12 0 2 62.69 3.41 1.4819 -6 2 3 62.96 2.02 1.4764 6 4 1 63.41 7.47 1.4670 7 3 2 63.51 3.96 1.4648 0 4 2 63.78 13.24 1.4593 -2 4 2 64.49 4.71 1.4450 14 0 0 64.72 3.03 1.4403 2 4 2 64.79 4.73 1.4389 8 4 0 65.10 1.41 1.4329 12 2 1 65.47 1.08 1.4256 -14 0 1 65.52 1.36 1.4246 -4 4 2 65.55 4.57 1.4241 -9 3 2 66.41 1.88 1.4078 1 3 3 66.47 1.82 1.4066 -8 4 1 66.47 2.15 1.4066 -3 3 3 68.18 7.50 1.3754 12 0 2 68.31 1.62 1.3732 8 4 1 68.46 1.31 1.3706 -13 1 2 68.54 2.01 1.3692 3 3 3 68.66 1.89 1.3669 -5 3 3 68.67 2.63 1.3667 -6 4 2 69.68 1.58 1.3495 9 3 2 70.11 2.48 1.3422 -2 0 4 70.30 6.75 1.3390 0 0 4 70.51 1.42 1.3356 14 2 0 70.65 3.18 1.3333 -3 5 1 71.20 1.45 1.3243 15 1 0 71.32 2.96 1.3224 3 5 1 71.33 1.14 1.3223 -4 0 4 71.38 2.21 1.3214 6 4 2 71.53 1.07 1.3190 -14 0 2 72.04 1.51 1.3109 5 3 3 72.23 1.60 1.3080 -7 3 3 72.23 1.02 1.3079 -11 3 2 72.56 4.18 1.3029 8 2 3 72.64 1.61 1.3016 -10 4 1 72.84 4.44 1.2985 -10 2 3 73.10 1.77 1.2946 13 3 0 73.23 3.15 1.2926 -5 5 1 74.27 1.59 1.2770 13 1 2 74.33 3.41 1.2761 5 5 1 74.85 1.66 1.2686 10 4 1 75.46 2.47 1.2598 7 5 0 76.11 1.12 1.2506 0 2 4 77.11 1.20 1.2369 -4 2 4 77.16 1.38 1.2362 -7 1 4 77.67 1.12 1.2294 2 2 4 77.76 1.50 1.2282 -15 1 2 78.28 1.63 1.2214 5 1 4 78.90 4.48 1.2133 -10 4 2 79.39 2.24 1.2070 10 2 3 79.73 2.21 1.2028 -12 2 3 79.96 1.40 1.1998 -12 4 1 80.01 1.23 1.1993 -5 5 2 80.83 1.43 1.1891 16 2 0 80.90 1.73 1.1882 9 5 0 81.38 1.12 1.1825 -16 0 2 81.72 1.89 1.1784 -9 1 4 82.15 1.26 1.1733 5 5 2 82.54 1.17 1.1688 12 4 1 82.64 2.53 1.1676 15 3 0 82.73 1.26 1.1665 0 6 0 82.74 1.20 1.1664 -17 1 1 83.18 1.77 1.1613 7 1 4 83.19 1.78 1.1613 10 4 2 83.40 1.37 1.1588 2 6 0 84.20 1.24 1.1499 15 1 2 84.72 1.97 1.1441 8 0 4 85.86 1.05 1.1319 -12 4 2 86.00 3.34 1.1304 2 6 1 86.36 1.51 1.1266 17 1 1 86.62 1.30 1.1239 18 0 0 86.97 1.15 1.1202 -16 2 2 87.36 1.57 1.1162 -4 6 1 87.41 2.83 1.1158 12 2 3 87.56 4.07 1.1142 14 4 0 87.60 1.54 1.1139 11 5 0 87.80 2.63 1.1118 -14 2 3 88.08 1.04 1.1090 -17 1 2 88.39 1.35 1.1059 -7 3 4 88.98 1.03 1.1001 -15 3 2 89.48 1.93 1.0952 5 3 4 ================================================================================ XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.