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dc.creatorŠajnović, Aleksandra
dc.creatorSimić, Vladimir
dc.creatorJovančićević, Branimir
dc.creatorCvetković, Olga
dc.creatorDimitrijevic, Radovan
dc.creatorGrubin, Nenad
dc.date.accessioned2018-11-22T00:12:38Z
dc.date.available2018-11-22T00:12:38Z
dc.date.issued2008
dc.identifier.issn1000-9515
dc.identifier.urihttp://cherry.chem.bg.ac.rs/handle/123456789/871
dc.description.abstractSediments of the western part of the Valjevo-Mionica basin (Serbia) were examined both geochemically and mineralogically to explain, on the basis of their sedimentological characteristics, the causes of changes in their qualitative and quantitative composition. A total of 62 samples obtained from the drillhole at depths up to 400 m was investigated. Using correlation of the obtained data, six geochemical zones were defined, two of which being specially distinguished by their mineralogical, geochemical and sedimentological characteristics. The first one, upper zone A, consists of banded marlstones interbedded with clay and oil shales and is characterized by presence of analcite and searlesite. These minerals and very high contents of Na(2)O indicate sedimentation in alkaline conditions with increased salinity in and climate. That provided pronounced water stratification, as well as higher bioproductivity in the basin and sedimentary organic matter preservation. Therefore, the zone A sediments are characterized by high organic matter contents of the type which provides good potential for production of liquid hydrocarbons. Another specific zone, zone F, contains sediments with very high MgO, K(2)O and Li concentrations. Their geochemical correlation, as well as almost complete absence of illite in this zone, indicates the presence of interstratified clay mineral type illite-saponite (lithium-bearing Mg-smectite).en
dc.publisherWiley-Blackwell Publishing, Inc, Malden
dc.relationMinistry of Science and Environmental Protection of the Government of the Republic of Serbia
dc.rightsrestrictedAccess
dc.sourceActa Geologica Sinica. English Edition
dc.subjectlacustrine sedimentsen
dc.subjectgeochemistryen
dc.subjectsearlesiteen
dc.subjectstatistical analysisen
dc.titleSedimentation History of Neogene Lacustrine Sediments of Suseocka Bela Stena Based on Geochemical Parameters (Valjevo-Mionica Basin, Serbia)en
dc.typearticle
dc.rights.licenseARR
dcterms.abstractСајновиц, Aлександра; Јованчићевић, Бранимир; Грубин, Ненад; Димитријевиц, Радован; Симиц, Владимир; Цветковиц, Олга;
dc.citation.volume82
dc.citation.issue6
dc.citation.spage1201
dc.citation.epage1212
dc.identifier.wos000262540000015
dc.citation.other82(6): 1201-1212
dc.citation.rankM22
dc.type.versionpublishedVersionen
dc.identifier.rcubKon_1824


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