Geological Society, London, Special Publications
Volume 372, 2013
Geological Development of Anatolia and the Easternmost Mediterranean Region
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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.