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dc.creatorRadosavljević, Slobodan
dc.creatorStojanović, Jovica
dc.creatorRadosavljević-Mihajlović, Ana
dc.creatorVuković, Nikola
dc.creatorMatijašević, Srđan
dc.creatorStojanović, Mirjana
dc.creatorKašić, Vladan
dc.date.accessioned2023-04-21T11:18:57Z
dc.date.available2023-04-21T11:18:57Z
dc.date.issued2014
dc.identifier.issn0350-0608
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/311
dc.description.abstractBased on geological, mineralogical, physical, chemical and technological investigations in the Tamnava Tertiary Basin near Šabac town (western Serbia), deposits of ceramic clays were studied. These ceramic clays are composed of kaolin-illite with a variable content of quartz, feldspars, mica, iron oxides and hydroxides, and organic matter. Four main types of commercial clays were identified: i) red-yellow sandy-gravely (brick clays); ii) grey-white poor sandy (ceramic clays); iii) dark-carbonaceous (ceramic clays); and iv) lamellar (“interspersed”) fatty, poor sandy (highly aluminous and ferrous clays). Ceramic clays are defined as medium to high plastic with different ranges of sintering temperatures, which makes them suitable for the production of various kinds of materials in the ceramic industry.en
dc.publisherUniverzitet u Beogradu - Rudarsko-geološki fakultet, Beograd
dc.relationinfo:eu-repo/grantAgreement/MESTD/Basic Research (BR or ON)/176016/RS//
dc.rightsopenAccess
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.sourceGeološki Anali Balkanskoga Poluostrva
dc.titleCeramic clays from the western part of the Tamnava Tertiary Basin, Serbia: Deposits and clay typesen
dc.typearticle
dc.rights.licenseBY
dc.citation.epage83
dc.citation.issue75
dc.citation.other2014(75): 75-83
dc.citation.rankM24
dc.citation.spage75
dc.citation.volume2014
dc.identifier.doi10.2298/GABP1475075R
dc.identifier.fulltexthttps://ritnms.itnms.ac.rs/bitstream/id/108/308.pdf
dc.identifier.rcubconv_1201
dc.type.versionpublishedVersion


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