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Cupromakovickyite |
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Topa D, Makovicky E, Balic-Zunic T |
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The Canadian Mineralogist 46 (2008) 515-523 |
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What is the reason for the doubled unit-cell volumes of |
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copper-lead-rich pavonite homologues? The crystal structures of |
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cupromakovickyite and makovickyite |
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Locality: Baita Bihor, Romania |
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_database_code_amcsd 0006187 |
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13.405 4.016 29.949 90 99.989 90 C2/m |
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atom x y z occ Uiso U(1,1) U(2,2) U(3,3) U(1,2) U(1,3) U(2,3) |
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Bi1 .34910 0 .46675 .834 .0211 .0187 .0222 .0218 0 .0020 0 |
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Ag1 .34910 0 .46675 .166 .0211 .0187 .0222 .0218 0 .0020 0 |
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Bi2 .44698 .5 .09518 .0179 .0197 .0209 .0133 0 .0033 0 |
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Bi3 .64982 0 .03264 .812 .0217 .0179 .0215 .0254 0 .0028 0 |
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Ag3 .64982 0 .03264 .188 .0217 .0179 .0215 .0254 0 .0028 0 |
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Bi4 .55023 .5 .40700 .834 .0204 .0207 .0232 .0170 0 .0029 0 |
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Ag4 .55023 .5 .40700 .166 .0204 .0207 .0232 .0170 0 .0029 0 |
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Bi5 .23915 0 .19489 .0207 .0154 .0266 .0179 0 -.0029 0 |
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Pb .74078 0 .32562 .0317 .0354 .0229 .0393 0 .0131 0 |
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Cu1 -.01975 .5 .21158 .0310 .017 .033 .040 0 -.005 0 |
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Cu2 .45067 .5 .27437 .0288 .021 .022 .040 0 -.006 0 |
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S1 .5 .5 0 .021 .023 .023 .015 0 -.0004 0 |
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S2 .40887 0 .38753 .018 .014 .020 .017 0 -.0009 0 |
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S3 .29366 0 .06067 .025 .021 .019 .035 0 .0003 0 |
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S4 .20840 .5 .43626 .024 .013 .016 .038 0 .005 0 |
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S5 .59356 0 .11343 .016 .017 .013 .015 0 -.011 0 |
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S6 .5 .5 .5 .023 .025 .021 .019 0 -.003 0 |
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S7 .14852 .5 .23335 .0134 .008 .017 .015 0 .002 0 |
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S8 .40537 .5 .17803 .0168 .019 .018 .0152 0 .008 0 |
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S9 .36457 0 .27147 .0123 .012 .015 .010 0 .002 0 |
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S10 .59796 .5 .32498 .0153 .013 .019 .015 0 .004 0 |
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