MC Göncüoğlu - Mineral resources of Turkey, 2019 - Springer
The geodynamic evolution of Turkey is mainly controlled by drift and collision of a number oceanic and continental plates or terranes. This can be ascribed to four orogenic episodes …
We present new, geological, metamorphic, geochemical and geochronological data on the East Anatolian–Lesser Caucasus ophiolites. These data are used in combination with a …
The plutonic units of the Elazığ magmatic complex crop out in the Pertek area of Tunceli Province (eastern Turkey) in the Southeast Anatolian Orogenic Belt (SAOB). Three stages of …
MA Erturk, M Beyarslan, SL Chung, TH Lin - Geoscience Frontiers, 2018 - Elsevier
The origin and geodynamic setting of the Maden Complex, which is situated in the Bitlis- Zagros Suture Zone in the Southeast Anatolian Orogenic Belt, is still controversial due to …
The remnants of the Southern Neotethys are represented by ophiolitic bodies and subduction/accretion complexes along the Southeast Anatolian-Zagros suture belt in the …
ABSTRACT The Southeast Anatolian Orogenic Belt (SAOB) is characterized by a tectonic assemblage consisting of dismembered ophiolites, subduction-related assemblages, and …
M Köküm - Journal of Structural Geology, 2024 - Elsevier
Abstract On 6 February 2023, the Elbistan (Kahramanmaraş)(Mw7. 6) earthquake produced a strike-slip type coseismic surface rupture zone, involving the sinistral slip of the …
Abstract During the Late Cretaceous in the Eastern Mediterranean, the northern branch of the southern Neotethys was closed by multiple northward subductions. Of these, the most …
Abstract The Southeast Anatolian Orogenic Belt (SAOB), the most extensive segment of the Alpine-Himalayan Orogenic Belt, resulted from the northward subduction of the southern …