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dc.contributor.authorHANİLÇİ, NURULLAH
dc.contributor.authorKaya, Mustafa
dc.contributor.authorKumral, Mustafa
dc.contributor.authorYalcin, Cihan
dc.date.accessioned2023-10-10T12:57:42Z
dc.date.available2023-10-10T12:57:42Z
dc.identifier.citationYalcin C., HANİLÇİ N., Kumral M., Kaya M., "Formation and tectonic evolution of structural slices in eastern Kargi Massif (Corum, Turkiye)", BULLETIN OF THE MINERAL RESEARCH AND EXPLORATION, ss.135-154, 2022
dc.identifier.issn0026-4563
dc.identifier.othervv_1032021
dc.identifier.otherav_294ceb2b-38e3-430f-83f0-3b0a3e567b1f
dc.identifier.urihttp://hdl.handle.net/20.500.12627/190349
dc.identifier.urihttps://avesis.istanbul.edu.tr/api/publication/294ceb2b-38e3-430f-83f0-3b0a3e567b1f/file
dc.identifier.urihttps://doi.org/10.19111/bulletinofmre.1067604
dc.description.abstractThe closure of Tethys Ocean has led to shaping the Central Pontides together with different types of rocks. In the east of Kargi (Gokcedogan), which is located in the Central Pontides, allochthonous rocks of Late Palaeozoic- Early Cenozoic age and autochthonous units exist together, and allochthonous rocks present various tectono-stratigraphical sequences. Distinctive tectonic slices developed in the area as a consequence of the thrusting of the Permian carbonates from the north towards the south over the Middle Jurassic accretionary Complex (Kunduz Metamorphites) that form the basement of the area, and also because of the thrusting of the units of the Kirazbasi Complex (ophiolitic melange) and Mesozoic carbonate rocks over this basement from the south towards the north because of the closure of Tethys Ocean. This paper presents whole-rock geochemical data, which suggest that the metabasites and the ophiolitic basalts are tholeiitic. The Jurassic metabasites from the Kunduz Unit and basalts from ophiolitic melange are characterized by the mid-ocean ridge basalt (MORB) and within plate tholeiites. This paper highlights the occurrence of the tectonic slices in the area is closely related to the tectonic evolution of the Tethys Ocean.
dc.language.isoeng
dc.subjectJeoloji
dc.subjectEkonomik Jeoloji
dc.subjectFizik Bilimleri
dc.subjectStratigrafi
dc.subjectGeoteknik Mühendisliği ve Mühendislik Jeolojisi
dc.subjectMühendislik ve Teknoloji
dc.subjectJeoloji Mühendisliği
dc.subjectJEOLOJİ
dc.subjectTemel Bilimler (SCI)
dc.subjectYerbilimleri
dc.subjectYER BİLİMİ, MULTİDİSİPLİNER
dc.titleFormation and tectonic evolution of structural slices in eastern Kargi Massif (Corum, Turkiye)
dc.typeMakale
dc.relation.journalBULLETIN OF THE MINERAL RESEARCH AND EXPLORATION
dc.contributor.departmentRepubl Turkiye Minist Ind & Technol , ,
dc.identifier.startpage135
dc.identifier.endpage154
dc.contributor.firstauthorID4312567


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