Strymon and Strymonikos Gulf basins (Northern Greece): Implications on their formation and evolution from faulting

▶ Stress-inverse methods for finding deformational path. ▶ Deformation of elastic material with “no memory”-co-axial stress and strain axes. ▶ Finding stress regime from heterogeneous fault-slip data. ▶ Wrench tectonics responsible for Strymon basin in the Hellenic hinterland.