Abstract
The Kizildağ ophiolite massif lies in the Hatay region of S. Turkey. Some structural relationships in the area are examined and two geological sections through the ophiolite are presented. A sequence of structural events, dealing with the emplacement and post-emplacement history, is established. The significance of the events is discussed and it is suggested that the post-emplacement structural history was dominated by movements along the Dead Sea Rift.
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