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...
I tiakina i:
| Ngā kaituhi matua: | , , , , , |
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| Hōputu: | Artigo |
| Reo: | Inglês |
| I whakaputaina: |
Faculty of Mining and Geology, Belgrade
2023-01-01
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| Rangatū: | Geološki Anali Balkanskoga Poluostrva |
| Ngā marau: | |
| Urunga tuihono: | https://doiserbia.nb.rs/img/doi/0350-0608/2023/0350-06082300009S.pdf |
| Ngā Tūtohu: |
Kāore He Tūtohu, Me noho koe te mea tuatahi ki te tūtohu i tēnei pūkete!
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