TURKISH JOURNAL OF EARTH SCIENCES, cilt.17, sa.3, ss.615-635, 2008 (SCI-Expanded)
In this paper, we aim to present stratigraphic and structural evidence for fault reactivation that is linked with evolution of the western part of the Manisa fault zone - a major range-bounding fault that is geomorphologically expressed as a trace of north-facing scarps bounding the southern margin of the Manisa basin which is subsidiary to the Gediz Graben.