The Pliocene–Quaternary tectonic evolution of the Cilicia and Adana basins, eastern Mediterranean: Special reference to the development of the Kozan Fault zone-Reference-Cited by-同舟云学术

The Pliocene–Quaternary tectonic evolution of the Cilicia and Adana basins, eastern Mediterranean: Special reference to the development of the Kozan Fault zone

Published:2014-05 Issue: Volume:622 Page:22-43
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

Aksu A.E.^ORCID,Walsh-Kennedy S.,Hall J.,Hiscott R.N.,Yaltırak C.,Akhun S.D.,Çifçi G.

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference54 articles.

1. Architecture of late orogenic basins in the eastern Mediterranean Sea;Aksu;Tectonophysics,1992

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

3. Neogene evolution of the Anaximander Mountains and Finike Basin at the Junction of Hellenic and Cyprus Arcs, Eastern Mediterranean;Aksu;Mar. Geol.,2009

4. Origin and evolution of the Neogene Iskenderun Basin, Northeastern Mediterranean Sea;Aksu;Mar. Geol.,2005

5. Complex fault interactions across an extensional imbricate fault fans developed in strike–slip settings: eastern Mediterranean Sea;Aksu;Mar. Geol.,2014

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