Yazar "Çimen, Okay" için listeleme
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Geochemical and radiometric data for mafic rocks from the Guleman Ophiolite (SE, Turkey): New insights on the geodynamic evolution of the southern Neo-Tethyan ocean
Sapancı, Özgür; Tokat, Gürkan; Eraslan, Nuh Kadr; Karakaya, Abdullah Onur; Gücer, Mehmet Ali; Çimen, Okay (Elsevier B.V., 2023)The Guleman Ophiolite is located in the southeast of Turkey and mainly consists of harzburgites and dunites hosting economically viable chromitite bodies, and lesser amounts of cumulate and isotropic gabbro, diabase dykes, ... -
Geochemical characteristics of microgranular enclaves in Early Eocene adakitic andesites (Gümüşhane, NE Türkiye)
Ali Gücer, Mehmet; Murat Güner, Abdulkadir; Çimen, Okay (Hacettepe Universitesi Yerbilmleri, 26 August )The early Cenozoic magmatism in the Eastern Sakarya Zone (NE Turkey) provides significant insights into the regional tectonomagmatic evolution. Adakite-like intrusive/extrusive rocks have been widely observed from the Late ... -
Geochronological and isotopic data from the adakitic Dodurga Pluton (Central Pontides, N Türkiye): new insights for the geodynamic evolution of the northern Neotethys
Çimen, Okay; Gücer, Mehmet Ali; Simonetti, Antonio; Karaoğlan, Fatih (TUBITAK, 2025)The Dodurga Pluton is located within the Central Pontides (northern Türkiye), has a SW–NE elongation, and consists of granodiorite and dacite porphyry. Previous studies have suggested that this pluton is Triassic in age, ... -
Revisiting the depositional age and provenance characteristics of metasedimentary rocks from the basement units in the Central Pontides (N Turkey): New constraints for tectonic evolution of the southern Black Sea region
Çimen, Okay; Akal, Cüneyt; Cemal Göncüoğlu, Mehmet; ARSLAN, Mehmet; Simonetti, Antonio; Karaoǧlan, Fatih (Elsevier Ltd, 1 May 2024)The pre-Jurassic tectonic evolution of the Central Pontides in northern Turkey is still poorly understood due to the lack of detailed geochemical and geochronological data from the basement units. Therefore, this study ...
