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dc.creatorStojanović, Jovica
dc.creatorRadosavljević, Slobodan
dc.creatorKaranović, Ljiljana
dc.creatorCvetković, Ljubomir
dc.date.accessioned2023-04-21T10:54:25Z
dc.date.available2023-04-21T10:54:25Z
dc.date.issued2006
dc.identifier.issn0077-7757
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/102
dc.description.abstractPolymetallic W-Pb-Bi ores have been found in the Nova jama ore zone of Rudnik Mt., Serbia. They are situated on the contact of quartzlatite dykes and breccias; mostly occur in a stockwork-type form. In this ore zone three mineralization phases can be distinguished: pyrometasomatic (skarn), pyrometasomatic-hydrothermal and hydrothermal. The pyrometasomatic-hydrothermal phase is the most significant mineralization phase because it is represented by massive ore bodies. They contain a wide variety of minerals including significant amounts of scheelite, native bismuth and sulphosalts, mostly presented by Pb-Bi-sulphosalts. Mo-free scheelite, the only tungsten bearing mineral, was found in economically interesting amounts. Energy Dispersive Spectrometry (EDS) analyses yielded the empirical formulae: Ca0.98WO4 for scheelite, Pb0.99S for galena, (Pb1.91Ag0.05Cu0.08)(2.04)Bi1.93S5 for cosalite and (Pb0.98Ag0.03Cu0.05)(1.06)Bi1.99S4 for galenobismutite. Tetragonal unit-cell parameters for scheelite amount to a = 5.24291 (6), c = 11.3738 (2) angstrom, V = 312.644 (7) angstrom(3). Atomic coordinates, isotropic displacement parameters, interatomic distances, and angles of scheelite were refined from X-ray powder diffraction data using the Rietveld method. Orthorhombic unit-cell parameters were calculated from single crystal data for cosalite to a = 19.13 (1), b = 23.64 (5), c 4.070 (3) angstrom, V = 1839 (5) angstrom(3) and for galenobismutite to a = 11.743 (3), b = 14.525 (8), c = 4.087 (8) angstrom, V = 696.0 (7) angstrom(3).en
dc.publisherE Schweizerbartsche Verlags, Stuttgart
dc.rightsrestrictedAccess
dc.sourceNeues Jahrbuch Fur Mineralogie-Abhandlungen
dc.subjectSerbiaen
dc.subjectscheeliteen
dc.subjectRudnik Mt.en
dc.subjectpyrometasomatic-high-temperature hydrothermal ore bodiesen
dc.subjectgalenobismutiteen
dc.subjectcosaliteen
dc.titleMineralogy of W-Pb-Bi ores from Rudnik Mt., Serbiaen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage306
dc.citation.issue3
dc.citation.other182(3): 299-306
dc.citation.rankM23
dc.citation.spage299
dc.citation.volume182
dc.identifier.doi10.1127/0077-7757/2006/0053
dc.identifier.rcubconv_516
dc.identifier.scopus2-s2.0-33748304337
dc.identifier.wos000240034700008
dc.type.versionpublishedVersion


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