Lower Palaeozoic-Paleogene geological development of a deep-water rift (Güzelsu Corridor) along the northern continental margin of the Southern Neotethys in the Eastern Mediterranean region: Evidence from the Antalya Complex and the adjacent Tauride Carbonate Platform-Reference-Cited by-同舟云学术

Lower Palaeozoic-Paleogene geological development of a deep-water rift (Güzelsu Corridor) along the northern continental margin of the Southern Neotethys in the Eastern Mediterranean region: Evidence from the Antalya Complex and the adjacent Tauride Carbonate Platform

Published:2024-05 Issue: Volume:252 Page:104741
ISSN:0012-8252
Container-title:Earth-Science Reviews
language:en
Short-container-title:Earth-Science Reviews

Author:

Robertson Alastair H.F.,Parlak Osman,Taslı Kemal,Solak Cemile,Dumitrica Paulian,Danelian Taniel

Funder

University of Edinburgh

Çukurova Üniversitesi

Mersin Üniversitesi

Publisher

Elsevier BV

Reference130 articles.

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4. Petrology of the Tekirova (Antalya) ophiolite (Southern Turkey): evidence for diverse magma generations and their tectonic implications during Neotethyan-subduction;Bağcı;Int. J. Earth Sci.,2009

5. Geochemical character and tectonic environment of ultramafic to mafic cumulates from the Tekirova (Antalya) ophiolite (Southern Turkey);Bağcı;Geol. J.,2006

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