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Paleoseismological features and tectonic setting of the Fethiye-Burdur fault zone (SW Turkey)

The Fethiye‐Burdur fault zone is not a single line. Still, it consists of discontinuous northeasterly trending fault segments developed parallel to each other between the Gulf of Fethiye and Burdur Lake. The NE‐trending and leftlateral oblique‐slip Fethiye‐Burdur fault zone bounds the Isparta Angle...

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Bibliografiska uppgifter
Huvudupphov: Sari Coşkun, Kamaci Zuheyr, Yağmurlu Fuzuli, Timur Emre, Şenturk Murat, Bozcu Mustafa
Materialtyp: Artigo
Språk:Inglês
Utgiven: Faculty of Mining and Geology, Belgrade 2023-01-01
Serie:Geološki Anali Balkanskoga Poluostrva
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Länkar:https://doiserbia.nb.rs/img/doi/0350-0608/2023/0350-06082300009S.pdf
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