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“Alpine type” Triassic of the Upper Antalya Nappe (Western Taurids—Turkey)

  • J. Marcoux
Conference paper
Part of the Schriftenreihe der Erdwissenschaftlichen Kommissionen book series (ERDWISSENSCHAFT, volume 2)

Abstract

The sections were made in the south-western branche of the Antalya nappes1). Structurally all of these sections belong to the highest unit of the Antalya nappes system. Stratigraphically this Triassic belong to shallow marine carbonate series, the recognized elements of which cover the stages between the Ordovician to the lower-middle Cretaceous. Certain outcrops show a continuous passage (without apparent unconformity), from a marine terminal Permian (Djulfian) to the lowest Triassic.

References

  1. 1) in J. H. Brunn and Al. Outline of the geology of the western Taurids — Pesl — Tripoli 1971.Google Scholar
  2. 2).
    in J. F. Dumont, M. Gutnic and Al. Le Trias des Taurides occidentales ... Z. Deutsch. Geol. Ges. Band 123, S. 385–409, Hannover 1972.Google Scholar

Copyright information

© Springer-Verlag Wien 1974

Authors and Affiliations

  • J. Marcoux
    • 1
    • 2
  1. 1.M. T. A. EnstitüsüAnkaraTurquie
  2. 2.C. N. R. S. ERA n° 9Laboratoire de Géologie Historique Bât 504OrsayFrance

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