Source to sink: The development of the latest Messinian to Pliocene–Quaternary Cilicia and Adana Basins and their linkages with the onland Mut Basin, eastern Mediterranean-Reference-Cited by-同舟云学术

Source to sink: The development of the latest Messinian to Pliocene–Quaternary Cilicia and Adana Basins and their linkages with the onland Mut Basin, eastern Mediterranean

Published:2014-05 Issue: Volume:622 Page:1-21
ISSN:0040-1951
Container-title:Tectonophysics
language:en
Short-container-title:Tectonophysics

Author:

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

Funder

Memorial University of Newfoundland

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geophysics

Reference63 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. The Cilicia–Adana Basin complex, Eastern Mediterranean: Neogene evolution of an active fore-arc basin in an obliquely convergent margin;Aksu;Mar. Geol.,2005

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

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

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