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Gulf Of Iskenderun
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Geologically, the Gulf is a classic example of a structural depression formed by the northward movement of the African tectonic plate relative to the Eurasian plate, specifically along the East Anatolian Fault System. Seismological data collected between 1985 and 2005 indicate an average westward tectonic drift rate of $2.1 \pm 0.3$ millimeters per year across the gulf's axial trough [2]. The seabed topography is characterized by a relatively shallow northern shelf, desc…