The origin of NE-trending basins and their relation to the E–W-trending grabens in western Turkey have been the subject of long lasting debate. The stratigraphical and structural …
B Uzel, H Soezbilir - Turkish Journal of Earth Sciences, 2008 - journals.tubitak.gov.tr
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 …
We present a compilation and comparison of geochemical data of Aegean Eocene to Recent magmatic rocks:(1) North Anatolian Eocene magmatic rocks (NAEM),(2) Aegean to …
V Işik, O Tekeli - International Journal of Earth Sciences, 2001 - Springer
The Simav metamorphic core complex of the northern Menderes massif, western Turkey, consists of a plutonic (Tertiary) and metamorphic (Precambrian) core (footwall) separated …
H Sözbilir - Geodinamica Acta, 2002 - Taylor & Francis
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 …
EY Ersoy, İ Çemen, C Helvacı, Z Billor - Tectonophysics, 2014 - Elsevier
The western part of the Aegean region includes several Neogene basins containing volcano- sedimentary successions. The Neogene basins, located along the northern Menderes …
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 …
Field studies on the Neogene successions in south of İzmir reveal that subsequent Neogene continental basins were developed in the region. Initially a vast lake basin was formed …
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 …