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In middle Miocene times, the collision between the Arabian microplate and Eurasia led to the separation between the Tethys and the Indian océans. This process resulted in profound changes in the oceanic circulation patterns, which shifted global climates towards colder conditions. The Hellenic arc, which has a land-locked configuration, underwent a widespréad extension for the last 20 Ma due to a slab roll-back process. In addition, the Hellenic Arc experienced a rapid rotation phase during the Pleistocene, with a counterclockwise component in its éastern portion and a clockwise trend in the western segment.