Add to ORKGThe tectonics of the Turkey is dominated by the collision between the Arabian and Eurasian plates. In this collision, the Bitlis Zagros Suture Zone is the most prominent tectonic structure. There exist metamorphics of the accretionary prism. Tectonic forces of the study area can be effective on thermal structure and mantle flow
The tectonic regime of Eastern Anatolia is determined by Arabian-Eurasian continentcontinent converg...
The geological setting of Turkey (figure 1)can be described as an assemblage of continental terranes...
We examined the thermal structure of the crust across complex deformation zones in SW Turkey using t...
Abstract The northeastern Turkey is located at the intensely deformed east Anatolian Collision Zone ...
The tectonic evolution of SE Anatolia is associated with the collision between the Taurides and the ...
Palaeomagnetic studies of the Neogene-Quaternary rocks of Anatolia have been mostly interpreted in t...
Inversion of the magnetotelluric data across the southwestern Taurides reveals two subzones of crust...
Turkey lies within the Alpine–Himalayan orogenic belt and is shaped by continent-continent collision...
Turkey forms one of the most actively deforming regions in the world and has a long history of devas...
The HarAYit granitoid in northeastern Turkey, comprises four separate granite units that are apparen...
Crustal and upper–mantle seismic discontinuities beneath eastern Turkey are imaged using teleseismic...
During the summer of 1996, wideband (0.003125-2000 s) magnetotelluric (MT) data were collected from ...
The Erzurum-Horasan-Pasinler basin, which surrounds Miocene rocks, is oriented approximately E-W and...
Geologic units of Bafa Lake and Akbuk Gulf, which have very importance in point of geologic and tect...
Detailed mapping near Sivrice shows that the northern margin of the Bitlis Suture zone consists of t...
The tectonic regime of Eastern Anatolia is determined by Arabian-Eurasian continentcontinent converg...
The geological setting of Turkey (figure 1)can be described as an assemblage of continental terranes...
We examined the thermal structure of the crust across complex deformation zones in SW Turkey using t...
Abstract The northeastern Turkey is located at the intensely deformed east Anatolian Collision Zone ...
The tectonic evolution of SE Anatolia is associated with the collision between the Taurides and the ...
Palaeomagnetic studies of the Neogene-Quaternary rocks of Anatolia have been mostly interpreted in t...
Inversion of the magnetotelluric data across the southwestern Taurides reveals two subzones of crust...
Turkey lies within the Alpine–Himalayan orogenic belt and is shaped by continent-continent collision...
Turkey forms one of the most actively deforming regions in the world and has a long history of devas...
The HarAYit granitoid in northeastern Turkey, comprises four separate granite units that are apparen...
Crustal and upper–mantle seismic discontinuities beneath eastern Turkey are imaged using teleseismic...
During the summer of 1996, wideband (0.003125-2000 s) magnetotelluric (MT) data were collected from ...
The Erzurum-Horasan-Pasinler basin, which surrounds Miocene rocks, is oriented approximately E-W and...
Geologic units of Bafa Lake and Akbuk Gulf, which have very importance in point of geologic and tect...
Detailed mapping near Sivrice shows that the northern margin of the Bitlis Suture zone consists of t...
The tectonic regime of Eastern Anatolia is determined by Arabian-Eurasian continentcontinent converg...
The geological setting of Turkey (figure 1)can be described as an assemblage of continental terranes...
We examined the thermal structure of the crust across complex deformation zones in SW Turkey using t...