“…The Grid Tomography is based on ray tracing techniques to compute the residual moveouts and takes information not only from geological consistent reflecting horizons, but also from local events, seismically coherent, interpretable just in restricted areas of the model. Also in this case, the possibility to depart from a definite horizons based model using further information from extra seismic events, gives the opportunity to highlight velocity anomalies in the updated velocity field often associated to pore pressure anomalies (Cibin P.2006, 2008, 2010and Colin Sayers, 2000.…”