Analytic signal representation of the synthetic seismogram of bright spots

Transformation of seismic signals into their analytic signal representation permits the unique separation of envelope, instantaneous phase, instantaneous frequency and apparent polarity. These parameters are useful in extracting the physical properties of a seismic signal and help in geophysical and geological interpretation. Deconvolution methods can improve the quality of the analytic seismic signal representation. From simulation studies it is found that time and space adaptive deconvolution significantly improves the quality of the analytic signal representation.