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dc.creatorRadosavljević, Slobodan
dc.creatorRakić, SM
dc.creatorStojanović, Jovica
dc.creatorRadosavljević-Mihajlović, Ana
dc.date.accessioned2023-04-21T10:51:49Z
dc.date.available2023-04-21T10:51:49Z
dc.date.issued2005
dc.identifier.issn0077-7757
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/80
dc.description.abstractThe mineral petrukite of stannite-like composition but different structure from Srebrenica orefield in eastern part of Bosnia and Herzegovina has been investigated. This mineral occurs in greisen-bordered sulphide veins in quartz-tourmaline rocks, which are almost completely replaced by a mean-temperature lead-antimony mineral paragenesis. The reflected light colour is brown-yellow. This mineral has a microhardness (VHN100) between 316 and 330 kp/mm(2). Results of an electron-microprobe analysis gave the average formula (Cu-1.96, Fe-0.98, Zn-0.09, Ag-0.09)(Sigma0.96) (Sn-0.94, In-0.02)(Sigma0.96), S-3.99. The strongest reflections in the X-ray powder pattern [d(in Angstrom)(1)] are: 3.124(100), 1.918(45), and 1.636(22). Orthorhombic unit cell parameters are: a = 7.677(4); b = 6.442(6); c = 6.264(3) Angstrom; V = 309.8(3) Angstrom(3).en
dc.publisherE Schweizerbartsche Verlagsbuchhandlung, Stuttgart
dc.rightsrestrictedAccess
dc.sourceNeues Jahrbuch Fur Mineralogie-Abhandlungen
dc.subjectSrebrenica orefielden
dc.subjectpetrukiteen
dc.subjectgreisenen
dc.subjectCu-Fe-Sn-S sulphosaltsen
dc.subjectBosnia and Herzegovinaen
dc.titleOccurrence of petrukite in Srebrenica orefield, Bosnia and Herzegovinaen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage26
dc.citation.issue1
dc.citation.other181(1): 21-26
dc.citation.rankM23
dc.citation.spage21
dc.citation.volume181
dc.identifier.doi10.1127/0077-7757/2005/0181-0008
dc.identifier.rcubconv_504
dc.identifier.scopus2-s2.0-13844250647
dc.identifier.wos000226937000003
dc.type.versionpublishedVersion


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