Clinozoisite Diffraction data computed using the structure from the paper listed below, along with the cell parameters refined from the powder pattern for R060284 Comodi P, Zanazzi P F American Mineralogist 82 (1997) 61-68 The pressure behavior of clinozoisite and zoisite: An X-ray diffraction study Sample: P = 42 kbar CELL PARAMETERS: 8.874000 5.593000 10.13900 90.00000 115.4000 90.00000 SPACE GROUP: P2_1/m X-RAY WAVELENGTH: 1.541838 2-THETA INTENSITY D-SPACING H K L 11.06 8.29 8.0187 1 0 0 17.71 28.54 5.0135 -1 0 2 18.58 4.42 4.7798 0 1 1 19.39 2.02 4.5821 -1 1 1 22.19 16.71 4.0093 2 0 0 22.34 14.01 3.9825 -2 0 2 23.72 7.02 3.7524 1 1 1 25.61 29.67 3.4797 -2 1 1 26.23 12.58 3.3988 1 0 2 27.87 14.61 3.2025 2 0 1 28.11 2.35 3.1752 -2 0 3 29.24 3.95 3.0549 0 0 3 30.56 1.49 2.9261 -3 0 1 30.64 18.91 2.9183 -3 0 2 30.92 100.00 2.8930 -1 1 3 31.96 37.48 2.8010 0 2 0 32.20 14.40 2.7802 2 1 1 32.42 2.51 2.7623 -2 1 3 33.41 27.73 2.6820 0 1 3 33.53 17.89 2.6729 3 0 0 33.90 18.09 2.6443 1 2 0 34.59 38.12 2.5936 -3 1 1 34.66 1.10 2.5881 -3 1 2 35.53 14.93 2.5269 2 0 2 35.84 5.32 2.5058 -1 0 4 36.76 12.12 2.4452 -1 2 2 37.49 27.02 2.3992 -3 1 3 37.64 23.12 2.3899 0 2 2 37.98 6.15 2.3690 -2 2 1 39.11 1.11 2.3034 2 1 2 39.23 4.44 2.2962 1 1 3 39.33 14.49 2.2911 -2 2 2 39.38 1.95 2.2881 -2 1 4 39.39 1.83 2.2874 -1 1 4 41.78 13.32 2.1619 -4 0 1 41.89 4.84 2.1563 -1 2 3 41.95 2.74 2.1534 -4 0 3 42.63 1.94 2.1207 0 1 4 42.89 20.59 2.1083 2 2 1 43.06 16.57 2.1005 -2 2 3 43.85 14.07 2.0645 0 2 3 43.86 2.10 2.0639 -4 1 2 44.33 6.39 2.0432 2 0 3 44.79 3.53 2.0234 -3 2 1 44.85 3.09 2.0208 -3 2 2 45.23 6.92 2.0047 4 0 0 45.61 1.59 1.9888 1 0 4 45.79 1.61 1.9814 -1 0 5 46.49 2.63 1.9530 -3 0 5 47.16 1.17 1.9269 -3 2 3 47.35 1.71 1.9195 2 1 3 48.51 9.09 1.8762 2 2 2 48.57 5.59 1.8742 1 1 4 48.74 3.29 1.8680 -1 1 5 48.74 14.44 1.8679 -2 2 4 48.75 5.23 1.8675 -1 2 4 49.01 3.34 1.8581 3 1 2 51.52 2.42 1.7734 0 2 4 51.65 3.91 1.7692 -5 0 2 52.21 1.12 1.7516 1 3 1 52.52 1.89 1.7421 0 1 5 52.59 1.73 1.7398 -4 2 2 53.20 3.27 1.7213 -2 3 1 53.79 6.46 1.7039 -4 1 5 53.94 1.58 1.6994 2 0 4 54.29 3.52 1.6892 -2 0 6 54.37 3.51 1.6871 -5 1 2 54.45 1.16 1.6845 -5 1 3 54.93 3.25 1.6712 -3 0 6 56.05 1.48 1.6403 1 0 5 56.25 13.37 1.6349 -5 1 1 56.24 9.72 1.6352 -1 0 6 56.27 11.42 1.6343 -1 3 3 56.43 3.53 1.6302 4 2 0 56.58 1.90 1.6262 2 1 4 56.70 13.91 1.6229 -4 2 4 56.75 8.34 1.6216 1 2 4 56.92 1.06 1.6172 -2 1 6 57.08 2.17 1.6131 2 3 1 57.15 3.48 1.6112 3 2 2 57.86 4.48 1.5933 0 3 3 58.08 12.54 1.5876 -4 0 6 58.62 6.68 1.5742 1 1 5 58.63 7.60 1.5741 -3 3 1 59.98 4.60 1.5418 5 1 0 60.08 5.08 1.5396 4 1 2 60.61 4.45 1.5274 -3 3 3 61.49 2.04 1.5075 -4 2 5 62.02 1.49 1.4958 -5 2 2 63.76 3.85 1.4591 -6 0 4 63.85 1.15 1.4574 3 0 4 64.00 10.64 1.4542 -5 2 4 64.07 3.27 1.4529 2 2 4 64.38 5.01 1.4465 -2 2 6 64.53 1.17 1.4436 3 2 3 64.96 7.92 1.4351 -3 2 6 65.76 1.79 1.4194 4 0 3 66.68 3.18 1.4021 2 1 5 66.77 22.31 1.4005 0 4 0 67.05 1.48 1.3952 -2 1 7 67.24 1.98 1.3918 5 2 0 67.33 15.32 1.3901 4 2 2 67.83 1.03 1.3812 -4 2 6 68.95 2.11 1.3613 1 3 4 69.95 1.79 1.3443 5 0 2 70.15 3.25 1.3410 0 2 6 72.15 1.88 1.3086 -6 2 3 72.87 1.17 1.2975 -5 2 6 72.91 3.46 1.2968 -6 2 2 73.09 2.47 1.2941 -6 2 4 73.25 2.11 1.2917 -4 3 5 73.74 1.68 1.2843 -5 3 2 73.82 1.20 1.2832 2 4 1 74.22 1.39 1.2772 3 0 5 74.37 1.84 1.2749 0 1 7 74.80 2.42 1.2687 -3 0 8 74.98 4.85 1.2661 4 2 3 75.16 1.21 1.2634 4 0 4 75.22 2.12 1.2626 -3 4 2 75.35 1.49 1.2608 -6 2 1 75.35 5.66 1.2609 -5 3 1 75.49 1.15 1.2587 2 0 6 75.70 5.64 1.2558 -6 2 5 75.91 1.49 1.2529 -2 0 8 76.80 2.44 1.2405 3 4 0 77.40 2.79 1.2324 1 3 5 77.96 3.32 1.2249 2 4 2 78.60 1.97 1.2166 5 3 0 78.68 1.77 1.2155 4 3 2 79.17 3.09 1.2092 -6 1 7 81.03 3.23 1.1861 0 2 7 81.92 1.58 1.1754 -4 4 1 84.31 1.32 1.1481 4 4 0 84.43 1.15 1.1467 -6 0 8 84.65 1.49 1.1444 2 3 5 86.72 2.82 1.1223 7 1 0 86.71 1.04 1.1224 0 1 8 87.42 1.91 1.1151 -7 1 7 87.84 1.66 1.1108 -5 2 8 87.91 1.42 1.1101 -1 2 8 87.91 1.42 1.1101 -1 2 8 XPOW Copyright 1993 Bob Downs, Ranjini Swaminathan and Kurt Bartelmehs For reference, see Downs et al. (1993) American Mineralogist 78, 1104-1107.