Some geological features of limestone aggregates produced from central anatolian carbonate formations

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dc.authorid0000-0002-3827-0941
dc.contributor.authorKansun, Gürsel
dc.contributor.authorZedef, Veysel
dc.contributor.authorKoçak, Kerim
dc.date.accessioned2020-03-26T19:45:16Z
dc.date.available2020-03-26T19:45:16Z
dc.date.issued2018
dc.departmentSelçuk Üniversitesi, Mühendislik Fakültesi, Jeoloji Mühendisliği Bölümüen_US
dc.description.abstractF or the last fifteen years, there has been extensive motorway and railway constructions in Turkey. This requires enormous amount of road-fillers and aggregates, and the construction companies open many open-pit limestone quarries to fulfill their aggregate needs. The partly double (four lines), partly one-way (double line) motorway of KonyaHüyük have recently been enlarged and partly re-constructed. During this construction, a total of five limestone quarry were opened to produce limestone aggregate. The Bozlutepe Limestone member of Asmalıtepe Formation near the town of Selki (HüyükKonya, central Anatolia) were used for this demand, and it has been operated for the last 6 years. The limestone member is approximately 200 m thick at most and mostly made of three type of minerals and these are dolomitic limestone, crystalline limestone and quartz-bearing crystallized limestones. All the minerals are crystallized and the minerals locally dominate at the quarry. The produced aggregates have relatively flat granulometry curve indicating most of the grains are of thin and have clay-silt sized particles. Our studies revealed that Bozlutepe Limestones are formed in carbonate facies in shallow marine environments during Permian-Carboniferous times. The member most likely have low-grade metamorphism during Paleozoic and Mesozoic erasen_US
dc.identifier.citationKansun, G. (2018). Some Geological Features of Limestone Aggregates Produced from Central Anatolian Carbonate Formations. Hittite Journal of Science and Engineering, 5(1), 57-61.
dc.identifier.endpage61en_US
dc.identifier.issn2149-2123en_US
dc.identifier.issn2148-4171en_US
dc.identifier.issue1en_US
dc.identifier.startpage57en_US
dc.identifier.urihttp://www.trdizin.gov.tr/publication/paper/detail/TWpjeU1qYzBOQT09
dc.identifier.urihttps://hdl.handle.net/20.500.12395/36014
dc.identifier.volume5en_US
dc.indekslendigikaynakTR-Dizinen_US
dc.institutionauthorKansun, Gürsel
dc.institutionauthorZedef, Veysel
dc.institutionauthorKoçak, Kerim
dc.language.isoenen_US
dc.relation.ispartofHittite Journal of Science and Engineeringen_US
dc.relation.publicationcategoryMakale - Ulusal Hakemli Dergi - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.titleSome geological features of limestone aggregates produced from central anatolian carbonate formationsen_US
dc.typeArticleen_US
dcterms.subjectLimestone aggregates
dcterms.subjectBozlutepe Limestones
dcterms.subjectGranulometry curves

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