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Makovickyite |
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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: Felbertal, Austria |
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13.239 4.0547 14.667 90 99.397 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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Cu1 .5 .189 .5 .384 .068 .020 .14 .043 0 .0002 0 |
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Cu2 -.0168 .0 .4448 .147 .070 .032 .09 .09 0 .006 0 |
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Ag .5 .0 .5 .280 .092 .10 .048 .10 0 .07 0 |
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Bi1 .15070 .0 .06591 .800 .0270 .0248 .0273 .0285 0 .0038 0 |
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Ag1 .15070 .0 .06591 .200 .0270 .0248 .0273 .0285 0 .0038 0 |
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Bi2 .44756 .0 .19061 .0277 .0287 .0292 .0252 0 .0041 0 |
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Bi3 .24868 .0 .62393 .0311 .0342 .0325 .0240 0 .0025 0 |
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S1 .5 .0 0 .0246 .028 .028 .017 0 .0008 0 |
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S2 .09017 .0 .22856 .0261 .023 .030 .024 0 .0008 0 |
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S3 .14326 .0 .45866 .0229 .022 .027 .018 0 .0006 0 |
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S4 .20751 .0 .87555 .0327 .024 .024 .047 0 .0032 0 |
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S5 .39748 .0 .35899 .0283 .033 .026 .029 0 .014 0 |
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