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This paper is focused on the main geological features of the Albanain Orogene. We seek to characterize the relation of this regional structure to the nearby regional tectonic units, summerizing its faulting patterns and the present neotectonic activity, as observed from the sesmic events and the geodynamic data. The geological structure of Albanides belongs to the Dinarides-Albanides-Hellenides folded belt, as an extension of the southern Mediterranean Alps. It extends along the eastern coasts of Adriatic and Ioni...