Makovickyite
Topa D, Makovicky E, Balic-Zunic T
The Canadian Mineralogist 46 (2008) 515-523
What is the reason for the doubled unit-cell volumes of
copper-lead-rich pavonite homologues? The crystal structures of
cupromakovickyite and makovickyite
Locality: Felbertal, Austria
_database_code_amcsd 0006188
13.239 4.0547 14.667 90 99.397 90 C2/m
atom      x    y      z  occ  Uiso U(1,1) U(2,2) U(3,3) U(1,2) U(1,3) U(2,3)
Cu1      .5 .189     .5 .384  .068   .020    .14   .043      0  .0002      0
Cu2  -.0168   .0  .4448 .147  .070   .032    .09    .09      0   .006      0
Ag       .5   .0     .5 .280  .092    .10   .048    .10      0    .07      0
Bi1  .15070   .0 .06591 .800 .0270  .0248  .0273  .0285      0  .0038      0
Ag1  .15070   .0 .06591 .200 .0270  .0248  .0273  .0285      0  .0038      0
Bi2  .44756   .0 .19061      .0277  .0287  .0292  .0252      0  .0041      0
Bi3  .24868   .0 .62393      .0311  .0342  .0325  .0240      0  .0025      0
S1       .5   .0      0      .0246   .028   .028   .017      0  .0008      0
S2   .09017   .0 .22856      .0261   .023   .030   .024      0  .0008      0
S3   .14326   .0 .45866      .0229   .022   .027   .018      0  .0006      0
S4   .20751   .0 .87555      .0327   .024   .024   .047      0  .0032      0
S5   .39748   .0 .35899      .0283   .033   .026   .029      0   .014      0