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dc.contributor.authorUnal, Neslihan
dc.contributor.authorHokerek, Selin
dc.contributor.authorAltunsoy, Mehmet
dc.contributor.authorOzcelik, Orhan
dc.contributor.authorErik, Nazan Yalcin
dc.contributor.editorBruckman, VJ
dc.contributor.editorHangx, S
dc.contributor.editorAsk, M
dc.date.accessioned2019-07-27T12:10:23Z
dc.date.accessioned2019-07-28T09:58:17Z
dc.date.available2019-07-27T12:10:23Z
dc.date.available2019-07-28T09:58:17Z
dc.date.issued2014
dc.identifier.issn1876-6102
dc.identifier.urihttps://dx.doi.org/10.1016/j.egypro.2014.10.360
dc.identifier.urihttps://hdl.handle.net/20.500.12418/8471
dc.descriptionGeneral Assembly of the EGU Division on Energy, Resources and the Environment (ERE) -- APR 27-MAY 02, 2014 -- Vienna, AUSTRIAen_US
dc.descriptionWOS: 000375918200020en_US
dc.description.abstractThe distribution values of m/z 191 triterpane and m/z 217 sterane of coaly Plio Miocene units determined by GC-MS were used to compare biomarker properties of Sahinali, Beypazan and Karapmar areas located in Aydin, Ankara and Konya (Turkey) regions within this study. In the Sahinali region the Miocene units consist of conglomerate, coal, clayey coal, sandstone, siltstone, claystone, clayey limestone and silicified limestone. Middle Upper Miocene units of the Beypazan Basin are represented by conglomerate, agglomerate, sandstone, siltstone, claystone, coal, bituminous shale, limestone, and tuff. The Pliocene Karapmar area of interest, which is characterized by sandstone, siltstone, claystone, mudstone, lake and river bed coal deposits. When all the biomarker values are considered, it can be concluded that the organic matter is not mature. In two areas except Sahinali gammacerane is present indicating salinity. According to the C-27, C-28 and C-29 sterane distribution, it can be observed that the dominant organic matter is terrestrial based and accompanied by simple herbaceous and alg. The deposition conditions are seen to be anoxic even though some oxic depositions are found in areas. All the areas had oleananes indicating angiosperm presence. C-29/C-30 hophane ratio and decrease in C-31-C-35 peak height indicated detrial facies in all the areas. (C) 2015 The Authors. Published by Elsevier Ltd.en_US
dc.description.sponsorshipEGU Diven_US
dc.language.isoengen_US
dc.publisherELSEVIER SCIENCE BVen_US
dc.relation.ispartofseriesEnergy Procedia
dc.relation.isversionof10.1016/j.egypro.2014.10.360en_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectPlio-Mioceneen_US
dc.subjectCoalen_US
dc.subjectBiomarkeren_US
dc.subjectGC-MSen_US
dc.subjectTurkeyen_US
dc.titleThe biomarker properties and comparisons of Sahinali, Beypazari and Karapmar (Turkey) coaly Plio-Miocene depositionsen_US
dc.typeconferenceObjecten_US
dc.relation.journalEUROPEAN GEOSCIENCES UNION GENERAL ASSEMBLY 2014, EGU DIVISION ENERGY, RESOURCES & THE ENVIRONMENT (ERE)en_US
dc.contributor.department[Unal, Neslihan -- Hokerek, Selin -- Altunsoy, Mehmet -- Ozcelik, Orhan] Akdeniz Univ, Dept Geol Engn, TR-07058 Antalya, Turkey -- [Erik, Nazan Yalcin] Cumhuriyet Univ, Dept Geol Engn, TR-58140 Sivas, Turkeyen_US
dc.identifier.volume59en_US
dc.identifier.endpage149en_US
dc.identifier.startpage142en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US


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