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dc.creatorGlumičić, T.L.
dc.creatorJovančićević, Branimir
dc.creatorMilojković, S.S.
dc.creatorNedeljković, J.M.
dc.creatorErcegovac, M.M.
dc.date.accessioned2018-11-22T00:01:03Z
dc.date.available2018-11-22T00:01:03Z
dc.date.issued1996
dc.identifier.issn0352-5139
dc.identifier.urihttps://cherry.chem.bg.ac.rs/handle/123456789/68
dc.description.abstractIn order to determine the origin of organic matter of Aleksinac oil shale (the village of Subotinac) a detailed GC-MS analysis of biological markers such as steranes, diterpanes and triterpanes was carried out. Also, micropetrographic analysis of samples was performed. The obtained results strongly suggest that the formation of the oil shale occurred in a large freshwater lake basin in which stratificaton of the water column was not possible, and that the majority of organic matter originates from algae, partially modified by microorganisms.en
dc.rightsrestrictedAccess
dc.rights.urihttps://creativecommons.org/licenses/by-nc-nd/4.0/
dc.sourceJournal of the Serbian Chemical Society
dc.subjectAleksinac oil shaleen
dc.subjectBiomarkersen
dc.subjectMicropetrographic analysisen
dc.subjectPrecursor biomassen
dc.titleInvestigation of the origin of Aleksinac oil shale organic matteren
dc.typearticle
dc.rights.licenseBY-NC-ND
dc.citation.volume61
dc.citation.issue11
dc.citation.spage1015
dc.citation.epage1024
dc.citation.other61(11): 1015-1024
dc.type.versionpublishedVersionen
dc.identifier.scopus2-s2.0-21444440257
dc.identifier.rcubhttps://hdl.handle.net/21.15107/rcub_cherry_68


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