2009-03-31, English, Article, Report edition: Syn-tectonic sedimentary evolution of the Miocene Catallar Basin, southwestern Turkey.(Report) Kosun, Erdal; Poisson, Andre; Ciner, Attila; ...

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Physical Description
  • Report
  • Magazine/​Journal article
Published
  • Elsevier B.V., 2009 March 31
Language
  • English

Edition details

Title
  • Syn-tectonic sedimentary evolution of the Miocene Catallar Basin, southwestern Turkey.(Report)
Also Titled
  • Syn-tectonic sedimentary evolution of the Miocene Catallar Basin, southwestern Turkey.
Appears In
  • Journal of Asian Earth Sciences, v.34, no.3, 2009 March 31, p.466(14) (ISSN: 1367-9120)
Author
  • Kosun, Erdal
  • Poisson, Andre
  • Ciner, Attila
  • Wernli, Roland
  • Monod, Olivier
Published
  • Elsevier B.V., 2009 March 31
Physical Description
  • Report
  • Magazine/​Journal article
Subjects
Target Audience
  • Academic
Summary
  • To link to full-text access for this article, visit this link: http:/​/​dx.doi.org/​10.1016/​j.jseaes.2008.07.005 Byline: Erdal Kosun (a), Andre Poisson (b), Attila Ciner (c)(e), Roland Wernli (d), Olivier Monod (e) Keywords: Sedimentology; Biostratigraphy; Source of detritals; Miocene; Basin analyses; Lycian Nappes Abstract: The Catallar Basin is one of the Miocene basins located in the southern part of the Bey DaAlari Massif (SW Turkey). This basin has been reinvestigated and new stratigraphic and sedimentological data are now presented. The Catallar Basin lies in paraconformity on the Bey DaAlari carbonate platform of Late Cretaceous to Palaeogene age. It consists of an impersistent, shallow-marine carbonate base (Karabayir formation, Late Oligocene to Early Burdigalian) followed by an onlapping detrital sequence including the Akcay and BaAbeleni formations (Langhian to Serravallian). The Akcay formation mainly contains turbidites in which several debris-flows and olistostromes are intercalated. The lowest debris flows derive from the local carbonate platforms of Cretaceous and Palaeogene age. Higher, the debris flows and olistostromes contain large carbonate blocks deriving from nearby sources (Bey DaAlari platform carbonates), whereas the accompanying pebbles originate from the allochthonous ophiolitic units located farther to the north (Lycian Nappes) or to the east (Antalya Nappes). The origin of these ophiolitic detritus is a matter of debate. The new data obtained in this study favour a northern origin. Author Affiliation: (a) Akdeniz University, Department of Geological Engineering, Merkez Kampus, 07000 Antalya, Turkey (b) Universite Paris-Sud, Sciences de la Terre, Batiment 504, 91405 Orsay Cedex, France (c) Hacettepe University, Department of Geological Engineering, Beytepe, 06800 Ankara, Turkey (d) Universite de Geneve, Geologie et Paleontologie, 13 rue des Maraichers, CH-1211 Geneve 4, Switzerland (e) Universite d'Orleans, ISTO, Geosciences, 45067 Orleans, France Article History: Received 5 June 2007; Revised 21 July 2008; Accepted 24 July 2008
Terms of Use
  • COPYRIGHT 2009 Elsevier B.V.
Language
  • English
Database
  • Gale Academic OneFile
Identifier
  • 350844814

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