Mineralogical and Petrographical Features of the Yarpuz (Kakliktas) Bauxite Deposit (Antalya/Turkey)

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dc.contributor.authorKaradağ, Mehmet Muzaffer
dc.date.accessioned2020-03-26T18:04:41Z
dc.date.available2020-03-26T18:04:41Z
dc.date.issued2010
dc.departmentSelçuk Üniversitesien_US
dc.description10th International Multidisciplinary Scientific GeoConference SGEM 2010 -- JUN 20-26, 2010 -- Albena, BULGARIAen_US
dc.description.abstractThe Yarpuz (Kakliktas) bauxite deposit is located in Antalya region southern Turkey; 35 km to the south of Seydisehir and 180 km to the north of Antalya. It is one of the bauxite deposits with the highest silica modulus (Al2O3%60.26 /SiO2%1.74=34.63) outcropping in the Central Taurus Mountains. The Upper Cretaceous Katrangedigi formation forms the basement and, comprises carbonate rocks. The bauxites were deposited in the palco-karstic depressions developed at the upper part of the Katrangedigi carbonate and, was overlain by the carbonate of the Upper Cretaceous (Senonien- Maestrichtien) Dogankuzu formation. The paleo-karstic depression bearing ore has a NE-SW aligment and ellipsoidal shape with 150 m of length and 30 m of width. Its average depth is 4 m and its deepest part is 12 m. The lense shaped ore deposit dips in accordance with the dip of limestone (N28(0)W, 28(0)SW). While the base of the ore deposit is highly irregular, its top is relatively flat. Bauxite cemented brecciated level (approximately 40 m) occur at the base of the ore deposit. With this shape, the ore deposit can be classified as pocket type allocton-semi allocton ore deposit. In the deposit, two types of elements, mostly massive and partially ferro bauxites have been identified. The massive bauxite is uniformly distributed within the deposit. Whereas, the ferro-bauxite is mainly condensed at the bottom of the deposit. The mineralogical analyses showed that the most common aluminum ore mineral is boehmite and, in lesser amount, diaspore and gibbsite accompany it. There are also kaolinite, hematite, goethite, pyrite, quartz, calcite, anatase (rare amount), rutile (rare amount), tridymite (rare amount) and, markazite, lepidocrocite, pyrolusite and psilomelane in very small amounts. Based on these data, the deposit is classified as boehmitic-type deposit.en_US
dc.description.sponsorshipMinist Environm & Water Bulgaria, Bulgarian Acad Sci, Acad Sci Czech Republ, Acad Sci IR Iran, Latvian Acad Sci, Polish Acad Sci, Russian Acad Sci, Serbian Acad Sci & Arts (SASA), Slovak Acad Sci, Natl Acad Sci Ukraine, Bulgarian Ind Assocen_US
dc.identifier.citationKaradağ, M. M., (2010). Mineralogical and Petrographical Features of the Yarpuz (Kakliktas) Bauxite Deposit (Antalya/Turkey). 10th International Multidisciplinary Scientific Geoconference: SGEM, 1, 105-120.
dc.identifier.endpage120en_US
dc.identifier.isbn978-954-91818-1-4
dc.identifier.issn1314-2704en_US
dc.identifier.startpage105en_US
dc.identifier.urihttps://hdl.handle.net/20.500.12395/25069
dc.identifier.wosWOS:000288623600015en_US
dc.identifier.wosqualityN/Aen_US
dc.indekslendigikaynakWeb of Scienceen_US
dc.institutionauthorKaradağ, Mehmet Muzaffer
dc.language.isoenen_US
dc.publisherINT SCIENTIFIC CONFERENCE SGEMen_US
dc.relation.ispartof10th International Multidisciplinary Scientific Geoconference: Sgemen_US
dc.relation.ispartofseriesInternational Multidisciplinary Scientific GeoConference-SGEM
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/closedAccessen_US
dc.selcuk20240510_oaigen_US
dc.subjectAksekien_US
dc.subjectbauxiteen_US
dc.subjectbohmiteen_US
dc.subjectkarsten_US
dc.subjectMiddle Tauridesen_US
dc.subjectmineralogyen_US
dc.subjectYarpuz-Turkeyen_US
dc.titleMineralogical and Petrographical Features of the Yarpuz (Kakliktas) Bauxite Deposit (Antalya/Turkey)en_US
dc.typeConference Objecten_US

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