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dc.creatorRadosavljević, Slobodan
dc.creatorĐorđević, Dragoslav
dc.creatorStojanović, Jovica
dc.creatorRadosavljević-Mihajlović, Ana
dc.creatorKasic, Vladan
dc.date.accessioned2023-04-21T11:18:20Z
dc.date.available2023-04-21T11:18:20Z
dc.date.issued2014
dc.identifier.issn1840-4855
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/306
dc.description.abstractThe Srebrenica orefield is mostly composed of Tertiary dacite-andesites, and quartz latites, pyroclastites, Paleozoic schists, and Quaternary sediments, but in a in a lesser extent. The latest research showed that in the Srebrenica orefield occur complex mineral parageneses and associations deposited in pneumatolytic-hydrothermal and hydrothermal (from high- to low-temperature) stage, accompanied with very rare minerals. Beside ore mineral parageneses and associations, specials emphasis was on rare hydrated phosphates: vivianite, ludlamite, and vauxite. It is important to say that vauxite from the Srebrenica orefield is fourth discovery in the world. The minerals above were studied using DTA-TGA, IR-spectroscopy, and XRPD.en
dc.publisherTechnical Inst Bijeljina, Bijeljina
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/176016/RS//
dc.rightsopenAccess
dc.sourceArchives for Technical Sciences
dc.subjectvivianiteen
dc.subjectvauxiteen
dc.subjectSrebrenica orefielden
dc.subjectRepublic of Srpskaen
dc.subjectmineralogyen
dc.subjectludlamiteen
dc.titleSrebrenica orefield, podrinje metallogenic district, Republic of Srpska, BiH: hydrated fe(al)-phosphates and their parageneses within the pb-zn mineralizationen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage6
dc.citation.issue11
dc.citation.other(11): 1-6
dc.citation.spage1
dc.identifier.doi10.7251/afts.2014.0611.001R
dc.identifier.rcubconv_834
dc.identifier.wos000445834500001
dc.type.versionpublishedVersion


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