The data presented in Table 1 are the final
displacements, after taking into account readings from
various stations, and their comparison to the modelled
ones. However, based on the time series of the closest
GPS stations, it seems that the displacement was not
instantaneous during the earthquake, but it was
stabilized after approximately two days. This gradual
evolution of the deformation can result from a
combination of the physical properties of the upper
crust and a triggered creep on secondary conjugate
strike-slip faults. The observed deformations in stations
located far from the epicentre have to be attributed to
random causes and are not been taken into account.