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The tectonic setting of Albania, influenced by the collision with the Adria microplate, is divided into two structural domains: an external compressional zone and an internal extensional one. Two main fault systems characterize the region-the longitudinal system (NW-SE to NNW-SSE), consisting of thrust and reverse faults, and the transversal system (NE-SW), comprising strike-slip faults. The Lushnje-Elbasan transverse fault, oriented NNE, is associated with the Dumrea diapiric dome and the Elbasan Quaternary grabe...