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

Author:

Hall J.,Aksu A.E.ORCID,Elitez I.ORCID,Yaltırak C.,Çifçi G.

Funder

Natural Sciences and Engineering Research Council of Canada (NSERC)

Dean of Science, Memorial University of Newfoundland

VP Research, Memorial University of Newfoundland

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference89 articles.

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2. Antalya Neojen havzasının stratigrafisi;Akay;Bull. Geol. Soc. Turk.,1985

3. Architecture of late orogenic Quaternary basins in northeastern Mediterranean Sea;Aksu;Tectonophysics,1992

4. Quaternary sedimentary history of Adana, Cilicia and Iskenderun Basins, northeastern Mediterranean Sea;Aksu;Mar. Geol.,1992

5. The Cilicia–Adana Basin complex, Eastern Mediterranean: Neogene evolution of an active fore-arc basin in an obliquely convergent margin;Aksu;Mar. Geol.,2005

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