Abstract

In 2D-3C and 3D-3C seismic data acquisition with SVSM digital sensor (Multicomponent sensor), where channels were more than 2000, a long felt need was to identify all the spiky traces and relate it with the objects on the ground within the short span of time. Number of times it was difficult to identify the source of spiky traces as the channel numbers were large and they were spread over a large, usually 30