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dc.contributorBalanović, Ljubiša
dc.contributorTanikić, Dejan
dc.creatorKašić, Vladan
dc.creatorRadosavljević-Mihajlović, Ana
dc.creatorStojanović, Jovica
dc.creatorMihajlović, Slavica
dc.creatorVukadinović, Melina
dc.creatorĐorđević, Nataša
dc.creatorJelić, Ivana
dc.date.accessioned2023-11-24T09:18:19Z
dc.date.available2023-11-24T09:18:19Z
dc.date.issued2023
dc.identifier.isbn978-86-6305-140-9
dc.identifier.urihttps://ritnms.itnms.ac.rs/handle/123456789/1177
dc.description.abstractZeolites are a group of natural and synthetic inorganic compounds. They have specific physicochemical properties suitable for industrial application [1,2]. According to their origin, variety of chemical composition, structural characteristics and application, zeolites form a specific group of minerals within the tectosilicates. In sedimentary formations rich in zeolites, the most characteristic minerals that are present are: clinoptilolite/hailandite, chabazite, mordenite, erionite, phillipsite and analcime. The most widespread zeolite of sedimentary origin is represented by the HEU series (clinoptilolite-heylandite). Its general crystal chemical formula is (Na,K,Ca)6Al6Si30O72nH2O.. Based on chemical and X-ray powder diffraction analysis, it is not possible to separate clinoptilolite and hoylandite . This is due to their isostructural nature. To identify these two isostructural minerals, even today, the simplest so-called Mampton's test [3]. Mumpton [4]. The results of X-ray diffraction analysis of thermally treated clinoptilolitic tuffs from the Zlatokop and Beočin deposits will be presented in this paper. The interplane distance values will be shown in the characteristic temperature range from 400oC to 500oC (when the first polymorphic transition occurs). These values characterize the zeolitic tuffs of our deposits in a certain way.sr
dc.language.isoensr
dc.publisherBor : University of Belgrade, Technical Faculty in Borsr
dc.publisherBor : Mining and Metallurgy Institute Borsr
dc.relationinfo:eu-repo/grantAgreement/MESTD/inst-2020/200023/RS//sr
dc.rightsopenAccesssr
dc.source54th INTERNATIONAL OCTOBER CONFERNCE on Mining and Metallurgysr
dc.subjectzeolitic tuffsr
dc.subjectX-ray powder analysissr
dc.subjectthermal stabilitysr
dc.titleSTUDY OF THERMALLY TREATED ZEOLITIC TUFFS OF SERBIA , DEPOSITS "ZLATOKOP" AND "OPĆIŠTE"-BEOČINsr
dc.typeconferenceObjectsr
dc.rights.licenseARRsr
dc.citation.epage352
dc.citation.spage348
dc.identifier.fulltexthttp://ritnms.itnms.ac.rs/bitstream/id/2706/bitstream_2706.pdf
dc.type.versionpublishedVersionsr


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