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SEDIMENTOLOGICAL ANALYSIS OF THE COAL IN THE WESTERN PART OF THE COAL BASIN KOSTOLAC (SERBIA)
Abstract
In this paper the results of sedimentological analysis of coal in 2010 at the lokality Petka (western coal basin Kostolac). Are presented variations of petrographic composition of coal matter (lithotypes, microlithotypes and macerals), mineral admixtures (clay, aleurite and marl) and locally occurring epigenetic mineralizations. The Kostolac Neogene Basin (Figure 1), cont aining three tick lignite beds of Pontian age[1] is one of important energetic resources of Serbia and is the bases for operating two lignite-firing electric power stations (K ostolac A and B). The eastern part of the basin is well geologicaly explored and there is the only one lignite producer in the basin – the open pit Drmno [4], but the western part of the basin has an important lignite potential. Coal of all three coal beds is typical lignite, built up by pices of coal matter of diverse strucures.
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References4
Dangic, A. & Dimitrijevic, D. 2001. Trace elements in lignites of the Kreka Basin (BiH) as possible contaminants of the e nvironment. Third International Symposium Mining and Envir. Protection, Belgrade, Proceedings, 387–391.
Dangic, A., Simonovic, Dimitrijevic, D. & Babovic, M. 2007. Kolubara lignite basin (Serbia): Importance of petrographic and geochemical studies to rational coal exploitation. Balkanmine 2007 - 2nd Balkan Mining Congress, Belgrade, Book of Proceedings, 9–14.
Krstic, S. 2010. Report about of sediment ological analyis samples of coal – western part Kostolac Basin. Mining and Metallurgy Institut in Bor, Zeleni Bulevar 35, Serbia.
Matic, V. i Glamocanin, L. 2008. Elaborat o rezervama uglja u lezistu Drmno. Tekstualni deo. Georad d.o.o.Drmno, 138 str.
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