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dc.creatorRadosavljević, Slobodan
dc.creatorStojanović, Jovica
dc.creatorRadosavljević-Mihajlović, Ana
dc.date.accessioned2023-04-21T10:53:57Z
dc.date.available2023-04-21T10:53:57Z
dc.date.issued2006
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/98
dc.description.abstractThe polymetallic W-Pb-Bi-Ag ore from the "Nova jama" ore zone of the Rudnik ore field have been investigated. Contact-pneumatolytic (skarn), pneumatolytic-hydrothermal, and hydrothermal mineralization phases are defined in this ore zone. The most significant mineralization phase that gave compact ore bodies is pneumatolytic-hydrothermal phase. A relatively pure Mo-free scheelite is the only tungsten-bearing mineral. Lead minerals are mostly presented by Pb-Bi sulphosalts and much less with galena. The image analysis coupled with Energy Dispersive Spectrometry (EDS) analysis on a Scanning Electron Microscope (SEM) was applied to the characterization of a W-Pb-Bi-Ag ore as an efficient tool for mineral quantification. Results of EDS (Energy Dispersive Spectrometry) analyses gave the empirical formulae: Pb 1.91 Ag 0.05 Cu 0.08 Bi 1.93 S 4 for cosalite, Pb 1.98 Ag 0.03 Cu 0.05 Bi 1.99 S 4 for galenobismutite and galena Pb 1.99 Ag 0.03 S.en
dc.publisherMinerals, Metals and Materials Society
dc.rightsrestrictedAccess
dc.sourceTMS Annual Meeting
dc.subjectScheeliteen
dc.subjectRudnik mineen
dc.subjectNative bismuthen
dc.subjectGalenobismutiteen
dc.subjectCosaliteen
dc.subjectCentral Serbiaen
dc.titleMineralogical and chemical characterization of the W-Pb-Bi-Ag ore from the Rudnik mine, Serbiaen
dc.typeconferenceObject
dc.rights.licenseARR
dc.citation.epage71
dc.citation.other2006: 65-71
dc.citation.spage65
dc.citation.volume2006
dc.identifier.rcubconv_1126
dc.identifier.scopus2-s2.0-33749254951
dc.type.versionpublishedVersion


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