1. n. [Geophysics]

The ability to distinguish between separate points or objects, such as sedimentary sequences in a seismic section. High frequency and short wavelengths provide better vertical and lateral resolution. Seismic processing can greatly affect resolution: deconvolution can improve vertical resolution by producing a broad bandwidth with high frequencies and a relatively compressed wavelet. Migration can improve lateral resolution by reducing the size of the Fresnel zone.

See: acquisition,  band,  deconvolution,  migration,  phase,  processing,  seismic modeling,  tuning effect,  water gun,  wavelet