▪ Abstract Dedicated to the memory of three pioneers, İhsan Ketin, Sırrı Erinç and Melih
Tokay, and a recent student, Aykut Barka, who burnt himself out in pursuit of the mysteries of …

Post-collisional magmatism may be generated by extensive crustal melting in Tibet-type
collisional environments or by falling out of slabs from under giant subduction–accretion …

SUMMARY The East Anatolian Fault (EAF) is a 700-km-long left-lateral transform fault
located between the Anatolian and Arabian plates. The proximity of the Euler Pole to the …

The Arabia‐Eurasia collision deforms an area of∼ 3,000,000 km2 of continental crust,
making it one of the largest regions of convergent deformation on Earth. There are now …

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 …

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 …

Watersheds are the fundamental organizing units in landscapes and thus the controls on
drainage divide location and mobility are an essential facet of landscape evolution …

The Lesser Caucasus occurs in the hinterland of the Arabia–Eurasia collision zone in the
broad Alpine–Himalayan orogenic belt and includes Cenozoic plutonic and volcanic …

Arabia–Eurasia convergence is achieved in the NW Zagros by a combination of shortening
on NW–SE-trending folds and thrusts, mainly in the Simple Folded Zone, and by right-lateral …

In this paper, we discuss the possibility that the North Anatolian fault (NAF) results from the
deep deformation of the slab beneath the Bitlis–Hellenic subduction zone. We described the …