The Denizli graben-horst system (DGHS) is located at the eastern-southeastern converging
tips of three well-identified major grabens, the Gediz, the Küçük Menderes and the Büyük …

İzmir Bay is an actively growing shallow marine basin controlled by active faults trending NE,
NW, NS and EW, in the West Anatolian Extensional Province. The bay of İzmir is a lazy L …

The Cumaovası basin, formerly known as the Çubukludağ Graben, is located at the western
end of Gediz and Küçük Menderes grabens in the west Anatolian extensional province. It is …

The study area is Nazilli-Buharkent section of the Büyük Menderes Graben. This is one of
the most active intracontinental extensional structures shaping the south-western Anatolian …

ABSTRACT The Kocaçay Basin (KÇB) is a key area in western Anatolia–a well‐known
extended terrane where regional segmentation has received limited attention–for …

Turkey is an area of complex geology with active tectonics and high geothermal potential.
Especially, the western part of Turkey is a region of abundant geothermal activity. Faults …

The structural evolution of the Miocene to Recent Gediz Graben is intimately related to the
evolution of its southern margin. This margin is shaped by a time‐transgressive, composite …

The Gediz Graben is a continental extensional basin filled with Miocene to Recent
sediments. The evolution of the graben can be expressed in terms of two phases:(i) Miocene …

Honaz Dağı (Honaz Mountain, Denizli) is the highest peak in western Anatolia (2517 m) and
represents the southern margin of the Denizli Graben Horst System in the western Anatolia …

Oblique and normal fault systems exposed in the Büyük Menderes Graben (BMG) region
record two successive and independent complex tectonic events. The first group tectonic …