2015
DOI: 10.1190/tle34040430.1
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Quality control of surface-consistent deconvolution on land dynamite data

Abstract: Seismic data with reliable amplitude and phase can significantly impact drilling programs by providing valuable descriptions of the reservoir and overburden, especially for complicated or subtle plays. Processing steps such as velocity tomography and amplitude-preserving migration are critical for producing high-quality seismic images, but equally important are surface-related premigration processing steps that can significantly alter seismic amplitude and phase information, such as deconvolution. During land … Show more

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Cited by 3 publications
(3 citation statements)
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“…The waveform of the transmitted signal can affect the resistance of the signal to surrounding or internal noises. Signals with zero phase in frequency domain are more resistant to phase distortion than non-zero-phase signals ( 33 , 34 ). A Ricker wavelet has a higher signal-to-noise ratio and spatial resolution as well as a lower power loss ( 31 ) than other wavelet shapes, such as Gaussian wavelet, Sine wavelet, and Raised cosine.…”
Section: Methodsmentioning
confidence: 99%
“…The waveform of the transmitted signal can affect the resistance of the signal to surrounding or internal noises. Signals with zero phase in frequency domain are more resistant to phase distortion than non-zero-phase signals ( 33 , 34 ). A Ricker wavelet has a higher signal-to-noise ratio and spatial resolution as well as a lower power loss ( 31 ) than other wavelet shapes, such as Gaussian wavelet, Sine wavelet, and Raised cosine.…”
Section: Methodsmentioning
confidence: 99%
“…In our workflow, the source wavelet is estimated from the surface-consistent deconvolution (Taner et al, 1981;Garceran et al, 2012;Zhang et al, 2015). In surfaceconsistent deconvolution, the recorded seismogram can be modeled as:…”
Section: Source Wavelet and Spatially-variant Waveformmentioning
confidence: 99%
“…Figure 1 shows the zero-lag cross-correlation of one crossspread between field data and synthetics based on FWI models up to 10 Hz. The similarity between the field data and the corresponding synthetic data is improved when two-term deconvolution (Zhang et al, 2015) is applied to the input field data prior to FWI.…”
Section: Source Wavelet and Spatially-variant Waveformmentioning
confidence: 99%