Petrolgy of the volcanic/subvolcanic members of the volcanosedimentary Maden Complex in Eastern Turkey

dc.authorid0000-0003-1694-0024en_US
dc.contributor.authorÖzdemir, Yavuz
dc.contributor.authorMercan, Çağrı
dc.contributor.authorOyan, Vural
dc.contributor.authorAtakul-Özdemir, Ayşe
dc.contributor.authorGüleç, Nilgün
dc.contributor.authorÖzkan-Altıner, Sevinç
dc.date.accessioned2023-05-24T09:57:43Z
dc.date.available2023-05-24T09:57:43Z
dc.date.issued2021en_US
dc.departmentMAÜ, Meslek Yüksekokulları, Savur Meslek Yüksekokulu, Harita ve Kadastro Bölümüen_US
dc.description.abstractMaden Complex exposed in Eastern Turkey, is a succession of volcano-sedimentary rocks and tectonically overlain by Bitlis Metamorphics and Cretaceous ophiolitic rocks. The succession includes shallow-water deposits and deep marine pelagic sediments intercalated with pillow lavas ranging from a few centimeters to ten meters in diameter. The planktonic foraminiferal assemblages from micritic limestones and zircon U-Pb ages from selected sedimentary rocks indicate the age of Late Ypresian - Early Lutetian. Plagioclase and clinopyroxenes are the main mineral phases, olivine rarely found as altered phenocrysts. Clinopyroxenes are augite and diopside, and their compositions are ranging between Wo44-51, En27-43, Fe10-21. The anorthite contents of plagioclases are between 32- 67 % in unaltered grains. The crystallization temperatures and pressures obtained from clinopyroxene chemistry are ranging from 1126 to 1250oC and 3 to 8 Kbar, respectively. The majority of the volcanic/subvolcanic rocks are subalkaline-tholeiitic basalts however; a few andesitic and rhyolitic derivatives are also present. The whole – rock and Sr-Nd-Pb isotope compositions reveal that the basaltic rocks are originated from E-MORB like asthenospheric mantle source without a subduction component.en_US
dc.identifier.doi10.5194/egusphere-egu21-15060en_US
dc.identifier.urihttps://doi.org/10.5194/egusphere-egu21-15060
dc.identifier.urihttps://hdl.handle.net/20.500.12514/3506
dc.language.isoenen_US
dc.publisherEGU General Assembly 2021en_US
dc.relation.ispartofEGU General Assembly 2021en_US
dc.relation.publicationcategoryKonferans Öğesi - Uluslararası - Kurum Öğretim Elemanıen_US
dc.rightsinfo:eu-repo/semantics/openAccessen_US
dc.subjectMaden Complexen_US
dc.subjectEastern Turkeyen_US
dc.titlePetrolgy of the volcanic/subvolcanic members of the volcanosedimentary Maden Complex in Eastern Turkeyen_US
dc.typeConference Objecten_US

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