At its most simple level, seismic interpretation involves tracing and correlating along continuous reflectors throughout the 3D dataset and using these as the basis for the geological interpretation, but the seismic dataset rarely gives a picture clear enough to do this.
At its most simple level, seismic interpretation involves tracing and correlating along continuous reflectors throughout the 2D or 3D dataset and using these as the basis for the geological interpretation. However, a seismic dataset rarely gives a picture clear enough to do this.