Abstract
Seismic moment values and fault plane solutions for large ( M s ⩾ 5.5) earthquakes which occurred in the Gulf of Corinth (central Greece) over the last 25 years, were used to calculate the average rate of deformation in the area. The results show north-south and east-west extension together with a downward movement of the northern side of the Gulf relative to the south at about 1 mm/yr.
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