The age and lithostratigraphic characteristics of Kumluca Zone, Alakırçay Group, SW Antalya-Turkey

A sedimentary unit, described in the literature as Alakırçay unit (Marcoux, 1977), Kumluca Zone (Robertson and Woodcock, 1981), Kumluca complex (Yılmaz, 1981) and Alakırçay group (Şenel et al., 1981) is exposed in a N-S trending area of 30 km x 4 km at SW of Antalya and N of Kumluca. The unit consists of sandstone with plant fragments, conglomerate, siltstone, claystone, limestone with Halobia and chert nodules and bedded cherts, and is of Triassic age according to Marcoux (1977), but a Ladinian-Norian age is given to it by Şenel et al. (1981).

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Marcoux, J., 1977, Geological sections of the Antalya region: Güvenç, T. and others, eds., Western Taurus excursion geological guidebook; VI. Colloquim on the geology of Aegean regions, Izmir.

Poisson, A., 1977, Recherches Geologiques dans les Taurides Occidentales (Turquie), These, L'Universite de ParisSud, Orsay, 795 pp.

Robertson, A.H.F. and Woodcock, N.H., 1981, Alakırçay Group, Antalya Complex, SW Turkey: A Deformed Mesozoic Margin: Sedimentary Geology, 30, 95-131.

Şenel, M.; Serdaroğlu, M.; Kengil, R.; Ünverdi, M. and Gözle, M.Z., 1981, Teke Torosları güneydoğusunun Jeolojisi: MTA Bull., 95/96, 13-43. Ankara-Turkey.

Yılmaz, P.O., 1981, Geology of the Antalya Complex, SW Turkey, (Ph. D. Dissertation): Austin, the University of Texas, University Microflims Inter., 268 p.