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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: acquisitionbanddeconvolutionmigrationphaseprocessingseismic modelingtuning effectwater gunwavelet

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