Age and kinematics of the Burdur Basin: Inferences for the existence of the Fethiye Burdur Fault Zone in SW Anatolia (Turkey)

ÖZKAPTAN M., KAYMAKCI N., Langereis C. G., Gulyuz E., ÖZACAR A. A., UZEL B., ...Daha Fazla

TECTONOPHYSICS, cilt.744, ss.256-274, 2018 (SCI-Expanded) identifier identifier

  • Yayın Türü: Makale / Tam Makale
  • Cilt numarası: 744
  • Basım Tarihi: 2018
  • Doi Numarası: 10.1016/j.tecto.2018.07.009
  • Dergi Adı: TECTONOPHYSICS
  • Derginin Tarandığı İndeksler: Science Citation Index Expanded (SCI-EXPANDED), Scopus
  • Sayfa Sayıları: ss.256-274
  • Anahtar Kelimeler: Burdur Basin, Fethiye-Burdur Fault Zone, Magnetostratigraphy, Anisotropy of Magnetic Susceptibility, Paleostress inversion, UPPER PLATE EXTENSION, QUATERNARY TECTONOSTRATIGRAPHIC EVOLUTION, ISPARTA ANGLE, SHEAR ZONE, PALEOMAGNETIC EVIDENCE, SOUTHWESTERN ANATOLIA, CAMELI BASIN, CYPRUS ARCS, MAGNETIC-SUSCEPTIBILITY, TECTONIC EVOLUTION
  • Orta Doğu Teknik Üniversitesi Adresli: Evet

Özet

The Burdur Basin is a late Miocene to Pliocene fluvio-lacustrine basin in SW Anatolia. It is developed within the postulated Fethiye-Burdur Fault Zone, which was argued to be a sinistral strike-slip fault zone developed in response to propagation of the Pliny-Strabo STEP fault into SW Anatolia (Turkey). In order to assess the presence and tectonic characteristics of the fault zone, we conducted a paleomagnetic study in the Burdur basin that involved rock magnetic experiments, Anisotropy of Magnetic Susceptibility (AMS) measurements and developing a magnetostratigraphy for dating purposes. The obtained age model constrains most part of the tectonic evolution of the basin. The well exposed (similar to 270 m thick) Burdur section revealed 3 normal and 2 reverse polarity magnetozones. We propose that the Burdur Formation spans most of the Gauss Chron (similar to 3.4-2.5 Ma) which implies a sedimentation rate of > 18 cm/kyr. The AMS results in the section indicate NW-SE directed extension.