The uppermost Messinian–Quaternary evolution of the Anamur–Kormakiti zone: The transition between the Outer Cilicia and Antalya basins, northeastern Mediterranean-Reference-Cited by-同舟云学术

The uppermost Messinian–Quaternary evolution of the Anamur–Kormakiti zone: The transition between the Outer Cilicia and Antalya basins, northeastern Mediterranean

Published:2022-02 Issue: Volume:136 Page:105451
ISSN:0264-8172
Container-title:Marine and Petroleum Geology
language:en
Short-container-title:Marine and Petroleum Geology

Author:

Aksu A.E.,Hall J.^ORCID,Yaltırak C.

Funder

Memorial University of Newfoundland

Natural Sciences and Engineering Research Council of Canada

Publisher

Elsevier BV

Subject

Stratigraphy,Economic Geology,Geology,Geophysics,Oceanography

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3. Complex interactions fault fans developed in a strike-slip system: Kozan fault zone, eastern Mediterranean Sea;Aksu;Mar. Geol.,2014

4. The pliocene-quaternary evolution of the Cilicia and Adana basins, eastern mediterranean: special reference to the development of the Kozan fault zone;Aksu;Tectonophysics,2014

5. Messinian evaporites across the anaximander Mountains, sırrı erinç plateau and the rhodes and finike basins, eastern Mediterranean Sea;Aksu;Mar. Geol.,2018

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