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1 CSIRO Minerals, Box 312, Clayton South, Victoria, 3169, Australia
2 Fachbereich Materialforschung und Physik, Universität Salzburg, Hellbrunnerstrasse 34, A–5020 Salzburg, Austria
3 Department of Geography and Geology, University of Copenhagen, Østervoldgade 10, DK–1350 Copenhagen, Denmark
E-mail address: emilm{at}geol.ku.dk
The crystal structure of proudite was redetermined with the holotype material from Tennant Creek, Australia, using a Nonius single-crystal diffractometer and MoK
radiation. Our determination of the structure, based on 3388 observed reflections, yielded an R1 value of 8.2% for 306 parameters. Proudite is monoclinic, a 31.814(1), b 4.1002(2), c 36.560(1), β 109.266(1)° and space group C2/m. Results of new electron-microprobe analyses give its composition as Cu1.9Ag0.1Pb15.6Bi20.4Sb0.1S32.4Se14.5. We report analytical data for associated phases and for Se-free proudite from Felbertal, Austria, as well. The crystal structure contains 18 large cation sites (Pb, Bi, and mixed positions), a single Cu site, and 24 anion sites, nearly all of them being mixed Se,S sites. It consists of regularly sheared double-layers of octahedra that alternate with stepwise sheared (100)PbS layers, two cation–anion sheets thick. Each straight portion of the former layers is 10 octahedra wide, whereas each straight interval of the PbS-like layers is eight square coordination pyramids (Pb, Bi) wide. Proudite is the highest known member of a homologous series of Pb–Bi– Cu sulfosalts with a mixed character, combining accretion of polyhedra and variable-fit of two layer-type fragments. This series contains proudite, felbertalite, makovickyite and a hypothetical intermediate member not yet known as a pure member, only as a combination with a "makovickyite-like element" in a synthetic selenide. This series is here defined as the proudite–felbertalite homologous series.
Keywords: proudite, crystal structure, proudite–felbertalite homologous series.
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