2012
DOI: 10.3997/2214-4609.20148302
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The Double Focal Transformation and its Application to Seismic Data Reconstruction

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Cited by 3 publications
(9 citation statements)
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“…Every row vector of R(zm) contains a convolution operator that applies the angle‐dependent reflection to the incident wavefield related to one spatial location. For more information about the reflectivity matrix, see Berkhout (), de Bruin, Wapenaar, and Breakout (), Doulgeris, Mahdad, and Blacquiere (), and Kutscha (). The reflected wavefield is then upward propagated to the receivers at the surface.…”
Section: Theory and Implementationmentioning
confidence: 99%
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“…Every row vector of R(zm) contains a convolution operator that applies the angle‐dependent reflection to the incident wavefield related to one spatial location. For more information about the reflectivity matrix, see Berkhout (), de Bruin, Wapenaar, and Breakout (), Doulgeris, Mahdad, and Blacquiere (), and Kutscha (). The reflected wavefield is then upward propagated to the receivers at the surface.…”
Section: Theory and Implementationmentioning
confidence: 99%
“…This would lead to a rough estimate of truex. Another possibility is to solve for truex by least squares (LS) inversion or by sparse inversion, which is also investigated in Kutscha and Verschuur () and Kutscha (). This paper will focus solely on the case of sparse inversion as this shows the best reconstruction results for coarse input data.…”
Section: The Double Focal Transformation As An Inverse Problemmentioning
confidence: 99%
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“…Conventionally, seismic processing is implemented as an open-loop process, in which information about the inconsistency between output and input is not taken into account. Recently, the so-called feedback-loop process has been introduced, see, e.g., Kutscha and Verschuur (2012) and Verschuur et al (2012) for data reconstruction, Lopez and Verschuur (2012) for multiple elimination and primary estimation, Soni et al (2012) and Davydenko et al (2012) for full wavefield migration, and Berkhout (2012) for joint migration inversion. The feedback-loop is described by an inversion problem of its own model parameters in each processing.…”
Section: Introductionmentioning
confidence: 99%