Eastern Anatolia is regarded as one of the best examples of continental collision,
represented by a 2 km high plateau. It displays shallow and diffuse seismicity, indicating that …

The East Anatolian High Plateau is a region of average∼ 2 km elevation asl exhibiting
active diffuse N‐S shortening and widespread Pliocene to recent volcanicity. Its elevation …

Lithospheric deformation throughout Anatolia, a part of the Alpine–Himalayan orogenic belt,
is controlled mainly by collision-related tectonic escape of the Anatolian Plate and …

The crustal structure of the Anatolian plateau in Eastern Turkey is investigated using
receiver functions obtained from the teleseismic recordings of a 29 broadband PASSCAL …

Crustal and upper-mantle seismic discontinuities beneath eastern Turkey are imaged using
teleseismic S-to-P converted phases. Three crustal phases are observed: the Moho with …

Eastern Anatolia is one of the best examples of an active continental collision zone in the
world. It comprises one of the high plateaus of the Alpine-Himalaya mountain belt, with an …

We use Pn phase travel time residuals to invert for mantle lid velocity and anisotropy
beneath northern Arabia‐eastern Anatolia continent‐continent collision zone. The primary …

The propagation characteristics of the regional Sn shear waves have been mapped to
provide insight into the lithospheric structure of the Anatolian and Iranian plateau and the …

Abstract The modern Anatolian–African plate boundary is represented by a north-dipping
subduction zone that has been part of a broad domain of regional convergence between …

We infer the lithospheric structure in eastern Turkey using teleseismic and regional events
recorded by 29 broad-band stations from the Eastern Turkey Seismic Experiment (ETSE) …