Browse

The seismicity of Albania is primarily driven by the collision between the Adria microplate and the Albanian orogen. The Ionian fault zone, located in southwestern Albania, is characterized by NW-SE trending neotectonic thrust faults with oblique components. These faults are predominantly marked by NW extension and include pre-Pliocene overthrust faults subjected to pure compressive stress. Occasionally, these overthrust faults are intersected by NE-SW-oriented thrust faults. The Ionian overthrust fault zone exten...

The orogeny in Albania and its surrounding, in collision with Adria microplate is divided in two domains of a different present-day tectonic regimes: the external domain with a compressional regime and the internal domain with an extensional regime. Two main fault systems are distinguished: 1) the longitudinal fault system, trending NW-SE up to NNW-SSE, represented by thrust and reverse faults, and 2) the traversal fault system NE-SW trending represented by strike-slip. The Lushnje-Elbasan transversal fault, in th...