Doi.org/10.1016/j.tecto.2014.05.002

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Revision as of 05:55, 18 August 2022 by 187.21.138.9 (talk) (Created page with "== Target Article == The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean. ; J. Hall, A.E. Aksu, İ. Elitez, C. Yaltırak, G. Çiftçi; Tectonophysics; 2014; https://doi.org/10.1016/j.tecto.2014.05.002 == Article providing comments == Reply to the comment by M.C. Alçiçek on “The Fethiye–Burdur Fault Zone: A component of upper plate extension o...")
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Target Article[edit | edit source]

The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean.  ; J. Hall, A.E. Aksu, İ. Elitez, C. Yaltırak, G. Çiftçi; Tectonophysics; 2014; https://doi.org/10.1016/j.tecto.2014.05.002

Article providing comments[edit | edit source]

Reply to the comment by M.C. Alçiçek on “The Fethiye–Burdur Fault Zone: A component of upper plate extension of the subduction transform edge propagator fault linking Hellenic and Cyprus Arcs, Eastern Mediterranean,” Tectonophysics, 635, 80–99, by J. Hall, A.E. Aksu, İ. Elitez, C. Yaltirak and G. Çi; Elitez, I.; Yaltırak, C.; Hall, J.; Aksu, A.E.; Çifçi, G.; ; Tectonophysics; 2015-11-01 https://doi.org/10.1016/j.tecto.2015.04.002

Summary[edit | edit source]

Note: Opened to append information.