To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the framework of Neotethyan subduction accommodating Africa-Eurasia convergence, we paleomagnetically assess the timing and amount of vertical axis rotations across the Uluklisla and Sivas regions. We show paleomagnetic results from ∼30 localities identifying a coherent rotation of a SE Anatolian rotating block comprised of the southern Klrisehir Block, the Uluklisla Basin, the Central and Eastern Taurides, and the southern part of the Sivas Basin. Using our new and published results, we compute an apparent polar wander path (APWP) for this block since the Late Cretaceous, showing that it experienced a ∼30-35° counterclockwise vertical axis rotation...
Western Anatolia is one of the world's most rapidly extending regions. The N-S extension commenced i...
Palaeomagnetic data on Eocene rocks from within the 'Almacik Flake', bounded by two strand...
The central Anatolia is comprises successor basins developed at the terminal phase of closure of Neo...
To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the fra...
To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the fra...
The Marmara region (northwestern Turkey) is located along the Alpine-Himalayan orogenic belt, and co...
Pliny-Strabo Trench is a Subduction Transform-Edge Propagator (STEP) Fault developed on the northern...
The central Anatolia comprises various continental fragments belonging to Laurasia at the north and ...
The tectonic evolution of SE Anatolia is associated with the collision between the Taurides and the ...
Paleomagnetism provides important constraints on complex patterns of vertical axis rotations in orog...
A paleomagnetic study of Cretaceous arc type rocks in the Central-Eastern Pontides and in the Southe...
Palaeomagnetic studies of the Neogene-Quaternary rocks of Anatolia have been mostly interpreted in t...
We have restored the geometries of suture zones that involved various continental blocks in central ...
The eastern Aegean region has undergone north dipping subduction in the Oligocene, continental colli...
Western Anatolia is one of the world's most rapidly extending regions. The N-S extension commenced i...
Palaeomagnetic data on Eocene rocks from within the 'Almacik Flake', bounded by two strand...
The central Anatolia is comprises successor basins developed at the terminal phase of closure of Neo...
To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the fra...
To quantitatively reconstruct the kinematic evolution of Central and Eastern Anatolia within the fra...
The Marmara region (northwestern Turkey) is located along the Alpine-Himalayan orogenic belt, and co...
Pliny-Strabo Trench is a Subduction Transform-Edge Propagator (STEP) Fault developed on the northern...
The central Anatolia comprises various continental fragments belonging to Laurasia at the north and ...
The tectonic evolution of SE Anatolia is associated with the collision between the Taurides and the ...
Paleomagnetism provides important constraints on complex patterns of vertical axis rotations in orog...
A paleomagnetic study of Cretaceous arc type rocks in the Central-Eastern Pontides and in the Southe...
Palaeomagnetic studies of the Neogene-Quaternary rocks of Anatolia have been mostly interpreted in t...
We have restored the geometries of suture zones that involved various continental blocks in central ...
The eastern Aegean region has undergone north dipping subduction in the Oligocene, continental colli...
Western Anatolia is one of the world's most rapidly extending regions. The N-S extension commenced i...
Palaeomagnetic data on Eocene rocks from within the 'Almacik Flake', bounded by two strand...
The central Anatolia is comprises successor basins developed at the terminal phase of closure of Neo...