2015
DOI: 10.1002/cjg2.20181
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A Stable and Efficient Attenuation Compensation Method based on Inversion

Abstract: Inverse Q filtering, which can compensate amplitude and correct phase, is an effective method to improve the resolution of seismic data. The conventional inverse Q method is usually based on wavefield continuation, which is unstable or under‐compensation. Based on the forward Q filtering equation in wavefield continuation, this work proposes a new attenuation compensation method, which is stable and accurate, taking advantages of the inverse theory and regularization strategy to obtain compensated seismic data… Show more

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Cited by 12 publications
(3 citation statements)
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“…For simplicity, Equation () is rewritten as bolddbadbreak=boldGm,$$\begin{equation}{{\bf d}} = {{\bf Gm}},\end{equation}$$where d is the observed non‐stationary seismic data, G is a forward operator containing attenuation information, m is the principal frequency spectrum of stationary data or compensated data. The compensated spectrum m 0 can be easily estimated via a damped least squares method (Wang et al., 2014): m0badbreak=false(GHboldG+λboldIfalse)1GHboldd,$$\begin{equation}{{{\bf m}}}_0 = {({{{\bf G}}}^H{{\bf G}} + \lambda {{\bf I}})}^{ - 1}{{{\bf G}}}^H{{\bf d}},\end{equation}$$where λ is a damping factor. Finally, the compensated spectrum m 0 is transformed to the time domain compensated signal via the inverse Fourier transform along the frequency axis.…”
Section: Methodsmentioning
confidence: 99%
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“…For simplicity, Equation () is rewritten as bolddbadbreak=boldGm,$$\begin{equation}{{\bf d}} = {{\bf Gm}},\end{equation}$$where d is the observed non‐stationary seismic data, G is a forward operator containing attenuation information, m is the principal frequency spectrum of stationary data or compensated data. The compensated spectrum m 0 can be easily estimated via a damped least squares method (Wang et al., 2014): m0badbreak=false(GHboldG+λboldIfalse)1GHboldd,$$\begin{equation}{{{\bf m}}}_0 = {({{{\bf G}}}^H{{\bf G}} + \lambda {{\bf I}})}^{ - 1}{{{\bf G}}}^H{{\bf d}},\end{equation}$$where λ is a damping factor. Finally, the compensated spectrum m 0 is transformed to the time domain compensated signal via the inverse Fourier transform along the frequency axis.…”
Section: Methodsmentioning
confidence: 99%
“…Next, the single‐channel compensation method using a damped least squares algorithm (Wang et al., 2014) and the proposed multichannel method are performed to compensate for the deep‐part energy of the noisy attenuated data and improve its vertical resolution. The compensated results of the single‐channel method are shown in the middle column of Figure 2.…”
Section: Examplesmentioning
confidence: 99%
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