Turkey forms one of the most actively deforming regions in the world and has a long history
of devastating earthquakes. The belter understanding of its neotectonic features and active …

To solve a long-lasting controversy on the timing and mechanism of generation of the
western Anatolian graben system, new data have been collected from a mapping project in …

The Menderes Massif covers large areas in western Turkey. The better understanding of its
tectono-metamorphic history would provide insight for the Alpine evolution of western Turkey …

The Büyük Menderes Graben is one of the most prominent structures of western Anatolia
(Turkey) and borders the Aegean. New structural and stratigraphic evidence demonstrates …

A close relationship between formation of approximately upright folds with axes normal to
the extension direction and ramp/flat extensional geometries is established for well exposed …

We have developed a significant body of new field-based evidence relating to the history of
crustal extension in western Turkey. We establish that two of the NE–SW-trending basins in …

Along the upper reaches of the Gediz River in western Turkey, in the eastern part of the
Aegean extensional province, the land surface has uplifted by∼ 400 m since the Middle …

The Alaşehir (Gediz) Graben exemplifies clastic sedimentation in a long-lived continental
half-graben in a semi-arid setting, developed within relatively incompetent metamorphic …

SUMMARY Aegean Graben System is a significant member of the complex geology of
western Turkey. The depths to the metamorphic basement reliefs in two major grabens have …

Small‐mammalian faunas enable the discrimination and correlation of uppermost Lower
Miocene lacustrine sedimentary units in central western Anatolia. On the basis of sequential …