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dc.creatorSekulić, Živko
dc.creatorMihajlović, Slavica
dc.creatorStojanović, Jovica
dc.creatorIvošević, Branislav
dc.creatorKašić, Vladan
dc.creatorIgnjatović, Miroslav R.
dc.date.accessioned2023-04-21T11:39:50Z
dc.date.available2023-04-21T11:39:50Z
dc.date.issued2019
dc.identifier.issn0860-7001
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/494
dc.description.abstractThis study shows the results of flotation concentration of mica minerals from kaolinised granite taken from the "Basica bare" deposit - Kobas, Srbac, The Republic of Srpska (B&H). Mineralogical composition of kaolinised granite is as follows: kaolinite, feldspar, quartz, and mica. After separating >0.630 mm, and LT 0.043 mm size class where kaolinite is concentrated, the rest is -0.630+0.043 mm class containing quartz, feldspar and mica. The mica concentrate was obtained by the flotation concentration, while feldspar and quartz were in the flotation underflow. According to the mineralogical analysis, the most abundant minerals are mica and chlorite/clays, while quartz and feldspar occur much less, and accessory minerals are represented in trace. The semi-quantitative mineralogical analysis obtained by the X-ray powder diffraction (XRPD) method of the mica concentrate amount to: mica approximate to 55%, chlorite/clays approximate to 35%, quartz approximate to 5%, feldspars (plagioclase and K-feldspars combined) approximate to 5%.en
dc.publisherPolska Akad Nauk, Polish Acad Sciences, Warszawa
dc.relationinfo:eu-repo/grantAgreement/MESTD/Technological Development (TD or TR)/34013/RS//
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/176016/RS//
dc.rightsrestrictedAccess
dc.sourceArchives of Mining Sciences
dc.subjectmuscoviteen
dc.subjectmica concentrateen
dc.subjectkaolinised graniteen
dc.subjectflotation concentrationen
dc.subjectbiotiteen
dc.titlePotentiality of obtaining mica flotation concentrate from kaolinised graniteen
dc.typearticle
dc.rights.licenseARR
dc.citation.epage508
dc.citation.issue3
dc.citation.other64(3): 499-508
dc.citation.rankM23
dc.citation.spage499
dc.citation.volume64
dc.identifier.doi10.24425/ams.2019.129365
dc.identifier.rcubconv_860
dc.identifier.scopus2-s2.0-85072630691
dc.identifier.wos000487581400003
dc.type.versionpublishedVersion


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