Abstract The Central and Eastern Anatolian plateaus are integral parts of the world's third
largest orogenic plateau. In the past decade, geophysical surveys have provided insights …

Geological and geomorphological offsets at different scales are used to constrain the
localization of deformation, total displacement, and slip rates over various timescales along …

The Tasova–Erbaa and Niksar basins are two adjacent pull-apart basins along the North
Anatolian Fault Zone (NAFZ). Within the Tasova–Erbaa basin, sedimentary lithofacies of the …

Surface uplift at the northern margin of the Central Anatolian Plateau (CAP) is integrally tied
to the evolution of the Central Pontides (CP), between the North Anatolian Fault (NAF) and …

A history of deformation has been determined for the Cameli Basin located in the western
part of the major Fethiye–Burdur Fault Zone, interpreted as the on-land continuation of Pliny …

SUMMARY The North Anatolian Fault (NAF) is a dextral strike-slip fault which runs about
1400 km from east to west, from the Karliova triple junction to the Aegean domain. It was …

Bu çalœ—mada, DoÕu Akdeniz bölgesinin kuzeydoÕu ucunda yer alan Hatay bölgesinde
Pliyo-Kuvaterner» den günümüze kadar etkin olan gerilme durumlarœ saptanmœ—tœr …

The North Anatolian Fault Zone is composed of two almost rectilinear branches which join in
a northward convex bend. In this bent zone, the Pontide-Anatolide collisional system has …

This study defines the Plio-Quaternary to present day stress regime in the Burdur Basin,
located at the northeastern end of the Fethiye–Burdur Fault Zone in SW Turkey. This fault …

In Anatolia, the late–post orogenic deformation is still continuing severely today. The north-
south compression initially deformed eastern Turkey. East and central Anatolia began to rise …