1963
DOI: 10.1190/1.1439310
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Wide‐band Velocity Filtering—the Pie‐slice Process

Abstract: A new technique has been developed which makes it possible to process a seismic record‐section in such a way that all seismic events with dips in a given range are preserved with no alteration over a wide frequency band, while all seismic events with dips outside the specified range are uniformly and severely attenuated. By applying this process to a noisy record‐section, a record‐section may be obtained which has all events within a specified dip range perfectly preserved, and very high‐velocity noise essenti… Show more

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Cited by 174 publications
(42 citation statements)
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“…The conventional methods can be divided into two groups. The first one can be summarized to filter method which is based on suppression of undesired parts of recorded data in the spectral domain, including high-pass and band-pass filtering, f − k filtering (Embree et al, 1963;Treitel et al, 1967;Yilmaz, 2001) and the adaptive ground-roll attenuation method (Wang et al, 2012;Hosseini et al, 2015). These methods have their limitations.…”
Section: Introductionmentioning
confidence: 99%
“…The conventional methods can be divided into two groups. The first one can be summarized to filter method which is based on suppression of undesired parts of recorded data in the spectral domain, including high-pass and band-pass filtering, f − k filtering (Embree et al, 1963;Treitel et al, 1967;Yilmaz, 2001) and the adaptive ground-roll attenuation method (Wang et al, 2012;Hosseini et al, 2015). These methods have their limitations.…”
Section: Introductionmentioning
confidence: 99%
“…Separating waves by velocity pass and reject filters is based on the following concept: waves which desired are signal and everything else is noise [9], [10] & [11]. So signal is passed by the time-correcting it for moveout and applying velocity pass filters that are centered about zero moveout.…”
Section: Fig8: Vertical Traces Of Vsp Data Snd-2 After True Amplitudmentioning
confidence: 99%
“…in seismic data, and f −k filtering is based on the dip of linear events (Embree et al, 1963). The recorded seismic data (P, the pressure field) are mapped from the time domain into the frequency-wavenumber domain through 2D Fourier transform.…”
Section: F − K Filteringmentioning
confidence: 99%