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January 01, 2013; Volume 372,Issue 1

Geological Development of Anatolia and the Easternmost Mediterranean Region

Editors: A. H. F. Robertson, University of Edinburgh, UK
O. Parlak, Çukurova University, Turkey and
U. C. Ünlügenç, Çukurova University, Turkey

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Hekimhan Basin, E Anatolia (looking E). Ophiolite-derived sediments, overlain by latest Cretaceous shallow-marine limestones (pale cliffs), with softer weathering Eocene marine sediments behind, in turn unconformably overlain by Plio-Quaternary basalts.

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