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dc.contributor.advisorBal Akkoca, Dicle
dc.contributor.authorBaytaşoğlu, Zeynep
dc.date.accessioned2020-12-29T12:54:29Z
dc.date.available2020-12-29T12:54:29Z
dc.date.submitted2011
dc.date.issued2018-08-06
dc.identifier.urihttps://acikbilim.yok.gov.tr/handle/20.500.12812/415320
dc.description.abstractÇalışmada Alibona Formasyonu alt seviyeleri, üst seviyeleri ve Malatya Volkanitleri'yle girik durumda bulunan göl çökellerinden örnekleme yapılarak, çökellerin mineraloji ve jeokimyasının belirlenmesi amaçlanmaktadır.
dc.description.abstractThe Permo-Triassic Keban Metamorphics are characterized by marble with schists. Alibonca Formation overlies Keban Metamorphics with angular unconformities, and represented by shallow marine clayey-carbonates and altered tuffs. Malatya Volcanics and volcano-sedimantary units show gradial transition to Alibonca, and have thick tuff levels, basaltic lavas and cherty limestones. Goal of this study 1-Ascertain of mineralogy and geochemistry of lower and upper levels of marine Alibonca Formation and Malatya lacustrine formation.en_US
dc.languageTurkish
dc.language.isotr
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAttribution 4.0 United Statestr_TR
dc.rights.urihttps://creativecommons.org/licenses/by/4.0/
dc.subjectJeoloji Mühendisliğitr_TR
dc.subjectGeological Engineeringen_US
dc.titleEski Arapgir (Malatya) civarındaki miyo-pliyosen birimlerin kil mineralojisi ve jeokimyası
dc.title.alternativeOld Arapgir (Malatya) mio-pliocene age around clay mineralogy and geochemistry of the units
dc.typemasterThesis
dc.date.updated2018-08-06
dc.contributor.departmentJeoloji Mühendisliği Anabilim Dalı
dc.identifier.yokid416801
dc.publisher.instituteFen Bilimleri Enstitüsü
dc.publisher.universityFIRAT ÜNİVERSİTESİ
dc.identifier.thesisid292710
dc.description.pages82
dc.publisher.disciplineDiğer


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