Miocene to Quaternary tectonostratigraphic evolution of the middle section of the Burdur-Fethiye Shear Zone, south-western Turkey: Implications for the wide inter-plate shear zones

İrem Elitez*, Cenk Yaltırak

*Bu çalışma için yazışmadan sorumlu yazar

Araştırma sonucu: Dergiye katkıMakalebilirkişi

25 Atıf (Scopus)

Özet

The Burdur-Fethiye Shear Zone (BFSZ) is a 75- to 90- km wide and 300-km-long transtensional left-lateral shear zone which is located in one of the most tectonically active regions in south-western Turkey. A considerable number of studies suggested contradictory models of the evolution and Neogene stratigraphy of the BFSZ and in most cases, the local river and alluvial fan deposits were mapped together with the lacustrine sediments and assigned a Pliocene age. We present new field data, fault kinematic analyses, and DEM and earthquake data to characterize the tectonic controls and extent of the middle section of the BFSZ including Acıpayam, Çameli and Gölhisar basins. Our field observations revealed two distinct sedimentary sequences that unconformably overlie the pre-Neogene basement. The first sequence begins with middle-upper Miocene meandering- and braided-river sediments of the Gölhisar Formation, which transition upward into lacustrine sediments of the upper Miocene-lower Pliocene İbecik Formation. This sequence is overlain by upper Pliocene-lower Quaternary alluvial fan conglomerates, mudstones and claystones of the Dirmil Formation. The basin deposits located in the middle section of the BFSZ consist of lacustrine sediments of a late Miocene lake that likely evaporated due to the Messinian salinity crisis. Fault kinematic analysis and DEM and earthquake data indicate that the middle BFSZ can be characterized as a heterogeneous left-lateral transtensional shear zone rather than a major fault system. Our findings suggest that the middle section of the BFSZ developed under the influence of progressive counter clockwise rotation of south-western Turkey, the Aegean graben system and the Cyprus and Hellenic arcs since the middle Miocene.

Orijinal dilİngilizce
Sayfa (başlangıç-bitiş)336-354
Sayfa sayısı19
DergiTectonophysics
Hacim690
DOI'lar
Yayın durumuYayınlandı - 28 Eki 2016

Bibliyografik not

Publisher Copyright:
© 2016 Elsevier B.V.

Finansman

This study is part of the ongoing Ph.D. studies of Elitez at Istanbul Technical University. The authors are grateful to TÜBİTAK ÇAYDAG (Project No: 107Y005 and 115Y424 ) and to the Istanbul Technical University Scientific Research Projects Coordination Department (Project No: 32511 ) for their financial support for the field studies. We thank Şükrü Özüdoğru and F. Eray Dökü for providing accommodation at the excavation of the ancient city of Kibyra. We thank Ali Aksu and Gürsel Sunal for their constructive comments. We also thank the reviewers and editor for helpful contributions to the manuscript.

FinansörlerFinansör numarası
Istanbul Technical University Scientific Research Projects Coordination Department32511
TÜBİTAK ÇAYDAG115Y424, 107Y005

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