title: Great Caucasus (Cavcasioni): A Long-lived North-Tethyan Back-Arc Basin
abstract: The Great Caucasus is a northwest-southeast-directed mountain range more than 1100 km long, located between the Black Sea and Caspian Sea. It represents an intracontinental tectonic system resulting from the Late Cenozoic structural inversion of a Palaeozoic-Mesozoic-Early Cenozoic back-arc basin (Dizi basin) in response to the convergence of the Africa-Arabian and Eurasian lithospheric plates. It is bounded to the south by the Transcaucasian massif, a palaeo-island-arc, and to the north by the 
journal: TURKISH JOURNAL OF EARTH SCIENCES