Deformation of the southern Aegean from continuous Global Positioning System measurements

The coseismic displacement derived from the GPS data were used to obtain estimates of the eqrthquake parameters. Okada model for single rectangular fault was used to model the surface displacements. The fault plane orientation (strike=332°, dip=6°, rake=120°), depth (20 km), and the fault dimensions (15.2×40.0 km) were kept fixed, the slip, latitude and longitude were varied. Kinematic detection of the earthquake