EARLY MIOCENE MILDLY-ALKALINE VOLCANISM IN THE KARACADAG AREA (CENTRAL ANATOLIA, TURKIYE)
dc.contributor.author | Asan, Kursad | |
dc.contributor.author | Kurt, Huseyin | |
dc.date.accessioned | 2020-03-26T17:38:17Z | |
dc.date.available | 2020-03-26T17:38:17Z | |
dc.date.issued | 2009 | |
dc.department | Selçuk Üniversitesi | en_US |
dc.description | 9th International Multidisciplinary Scientific Geo-Conference and Expo -- JUN 14-19, 2009 -- Albena, BULGARIA | en_US |
dc.description.abstract | In the Karacadag area (Central Anatolia, Turkiye), small volumes of mildly-alkaline lavas associated with large volumes of calcalkaline lavas crop out. 40Ar/39Ar age data indicate that the mildly-alkaline lavas were erupted during Early Miocene (ca. 18 Ma). The lavas are composed of alkali basalt, hawaiite, mugearite, benmoreite and trachydacite, and include olivine, ortho/clinopyroxene, amphibole, plagioclase, opaque and rare anorthoclase. The mildly-alkaline lavas have a sodic tendency (Na2O/K2O = 1.5-3.2) and resemble those of within-plate lavas. Alkali basalts of the suite were derived from a heterogeneous mantle source which is lithospheric mantle previously enriched by small degree melts from the astenosphere, plus possibly a depleted asthenospheric mantle. Melting modeling based on REE indicates that alkali basalts formed by 1-5 % partial melting of a spinet lherzolithic mantle source. Also, petrologic modeling based on trace element and isotopic data shows that fractional crystallisation played an important role in the evolution of the mildly-alkaline suite than AFC (assimilation and fractional crystallisation). | en_US |
dc.description.sponsorship | Minist Environm & Water, Bulgaria, Bulgarian Acad Sci, Acad Sci Czech Republic, Acad Sci IR Iran, Latvian Acad Sci, Polish Acad Sci, Russian Acad Sci, Serbian Acad Sci & Arts, Slovak Acad Sci, Natl Acad Sci Ukraine, Bulgarian Ind Assoc | en_US |
dc.identifier.endpage | 15 | en_US |
dc.identifier.scopusquality | N/A | en_US |
dc.identifier.startpage | 15 | en_US |
dc.identifier.uri | https://hdl.handle.net/20.500.12395/23435 | |
dc.identifier.wos | WOS:000276074500003 | en_US |
dc.identifier.wosquality | N/A | en_US |
dc.indekslendigikaynak | Web of Science | en_US |
dc.indekslendigikaynak | Scopus | en_US |
dc.language.iso | en | en_US |
dc.publisher | INT SCIENTIFIC CONFERENCE SGEM | en_US |
dc.relation.ispartof | SGEM 2009: 9TH INTERNATIONAL MULTIDISCIPLINARY SCIENTIFIC GEOCONFERENCE, VOL I, CONFERENCE PROCEEDING: MODERN MANAGEMENT OF MINE PRODUCING, GEOLOGY AND ENVIRONMENTAL PROTECTION | en_US |
dc.relation.publicationcategory | Konferans Öğesi - Uluslararası - Kurum Öğretim Elemanı | en_US |
dc.rights | info:eu-repo/semantics/closedAccess | en_US |
dc.selcuk | 20240510_oaig | en_US |
dc.subject | Central Anatolia | en_US |
dc.subject | Karacadag Alkaline | en_US |
dc.subject | Petrologic modeling | en_US |
dc.title | EARLY MIOCENE MILDLY-ALKALINE VOLCANISM IN THE KARACADAG AREA (CENTRAL ANATOLIA, TURKIYE) | en_US |
dc.type | Conference Object | en_US |