Abstract:

The Fethiye-Burdur Fay Zone, which forms the eastern border of the western Anadolu extension area, is an active Fay Zone, which runs from the Gulf of Fethiye in the south and extends to the Tea (Afyon) in the north, with a length of approximately 310 km, the KDGB goes to the left, with the form of the normal and normal benefits. The purpose of this study is to study the geological and neotectonic characteristics of the remaining section between Burdur-Kozluca in the north of the zone. The geology of the area of examination is separated by angle incompatibilities, the Late Trias-Late Cretace forms the old basin rocks, the Late Miyosen-Late Pleyistosen old basin rocks, and the Kuvaterner old young basin rocks. The old basin is formed by the Tefenni formation, which contains a deformed sedimentary resonance in the deformed lake environment with the Burdur formation and the alivial variety of deformations. Young swimming pools are made up of no deformation alivial range, hanged terrace and current flow sediments. The most important structural elements within the work area of the Fethiye-Burdur Fay Zone are the KD-GB extended Burdur Pool and the left side shape that limits this pool are the normal Burdur and Karakent benefits. In addition to these large-scale benefits that play an important role in the development of today's Burdur Basin, in the field of study, the KD-GB and KB-GD extended left side forms normal and normal benefits and the KD-GB, KB-GD and K-G extended small-scale normal benefits have also developed in late Miyosen-Pliyosen old falls. Structural analyses show that the region is now dominated by the KB-GD-oriented retreat regime.

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