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Claerbout's U/D principle

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Journal Article
Journal: Geophysics
Published: 01 June 1999
Geophysics (1999) 64 (3): 925–933.
... U/D principle. For both implementations, the impulse response is accurate up to 80 degrees from the vertical. Using synthetic data from a simple fault model, we test the depth migration scheme in the presence of lateral velocity variations. The results show that the proposed migration scheme images...
Series: Society of Exploration Geophysicists Geophysics Reprint Series
Published: 01 January 2008
EISBN: 9781560801924
... be obtained straightforwardly from the principle of conservation of acoustic power. In this paper I briefly review this derivation and show that the 3D generalization can be obtained along the same lines using a power reciprocity theorem. The resulting expression confirms Claerbout’s conjecture...
FIGURES
Series: Society of Exploration Geophysicists Geophysics Reprint Series
Published: 01 January 2016
EISBN: 9781560803188
... field can be reconstructed by the Kirchhoff integral, and the resultant reflector images are meaningful to within the validity of Claerbout’s Principle (see Claerbout, 1971; Claerbout and Doherty, 1972). Appendix B is devoted to a further discussion of this point. Figure 2. Photograph of 3-D...
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Journal Article
Journal: Geophysics
Published: 01 January 2003
Geophysics (2003) 68 (5): 1756–1759.
... be obtained straightforwardly from the principle of conservation of acoustic power. In this paper I briefly review this derivation and show that the 3D generalization can be obtained along the same lines using a power reciprocity theorem. The resulting expression confirms Claerbout's conjecture...
FIGURES
Journal Article
Journal: Geophysics
Published: 26 October 2007
Geophysics (2007) 72 (6): S221–S230.
... of x . Therefore, stacking the common-shot and common-receiver images reduces the influence of the coverage. The classic imaging principle ( Claerbout, 1971 ) defines the common-shot image by (A-1) I C ( x s , x ) = 1 A ( x s , x ) ∫ ω min ω max d...
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Journal Article
Journal: Geophysics
Published: 15 October 2008
Geophysics (2008) 73 (6): S219–S227.
... ratio ( Claerbout, 1971 ); i.e., (7) R ( x , y , z ) = ∑ j = 1 N ω P U ( x , y , z ; ω j ) P D ( x , y , z ; ω j ) , where N ω is the number of frequencies used in the process. Because the reflector position...
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Journal Article
Journal: Geophysics
Published: 30 May 2016
Geophysics (2016) 81 (4): V283–V302.
... time migration (RTM) methods, for two-way propagating waves, are extensions and/or variants of the second of Claerbout’s imaging conditions, and do not correspond to Claerbout’s imaging condition III. Variants and extensions of the original Claerbout II imaging principle (see, e.g., Zhang et al...
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Journal Article
Journal: The Leading Edge
Published: 01 July 2015
The Leading Edge (2015) 34 (7): 814–816.
... coincidence of upgoing and downgoing waves): (1) (2) In equations 1 and 2 , D ( x → , x → s ; ω) and U ( x → , x → s ; ω) represent downgoing and upgoing wavefields, respectively, and * represents the complex conjugate. The test data...
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Journal Article
Journal: Geophysics
Published: 17 August 2006
Geophysics (2006) 71 (4): SI103–SI110.
... methods to work well. This is difficult in areas with severe statics problems that preclude effective velocity analysis. 08 04 2005 21 10 2005 Figure 1. Deviated VSP geometry, where upgoing events U ( g ′ ∣ s ) from below the drillstring and downgoing events D...
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Journal Article
Journal: Geophysics
Published: 14 September 2010
Geophysics (2010) 75 (5): 75A195–75A209.
... ). Frasier (1970) generalizes Claerbout's result for obliquely propagating plane P- and SV-waves in a horizontally layered elastic medium. Analogous to equations 5 7 , equation 8 can be modified for transient or noise signals. For example, let u ( t ) = T ( t ) ∗ N ( t...
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Journal Article
Journal: Geophysics
Published: 01 January 2003
Geophysics (2003) 68 (2): 629–633.
... are, respectively, (4a) (4b) Expressed as functions of angular frequency ω = 2π f and wavenumber k x these are (5a) (5b) Inverse Fourier transformation of ( k x , z = 0, ω) and ( k x , z = 0, ω) from wavenumber k x to space x yields wavefields D ( x , z = 0, ω) and U...
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Journal Article
Journal: The Leading Edge
Published: 01 July 2015
The Leading Edge (2015) 34 (7): 808–813.
... that contribute to imaging and inversion and are considered to be signal, whereas multiples are not. Claerbout's imaging condition II, the time-and-space coincidence of upgoing and downgoing waves, is formulated as (3) where D is the downgoing wave and U is the upgoing wave, respectively...
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Journal Article
Journal: Geophysics
Published: 08 December 2010
Geophysics (2010) 75 (6): V111–V118.
... wavefield upward toward the sea surface ( Claerbout, 1976 ; Gazdag, 1978 ; Berkhout, 1982 ): (3) U ̃ ( k x , z 0 , ω ) = U ̃ ( k x , z R , ω ) exp [ i k z ( z 0 − z R ) ] , (4) D ̃ ( k x , z 0 , ω ) = D...
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Journal Article
Journal: Geophysics
Published: 15 December 2009
Geophysics (2009) 74 (6): WCA19–WCA34.
... modeling operator equations 5 and 6 F ¯ Shot-geophone modeling operator equations 9 and 10 F ¯ z Restricted modeling operator equations 25 and 26 w s Source field 18 u * Adjoint field 19 D , D ¯ Sunken survey 32...
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Journal Article
Journal: Geophysics
Published: 10 February 2022
Geophysics (2022) 87 (2): S53–S62.
... Reverse time migration (RTM) is an advanced technology used to image the interior of the Earth ( Baysal et al., 1983 ; McMechan, 1983 ; Whitmore, 1983 ; Levin, 1984 ). The RTM technique uses Claerbout’s (1971) imaging principle, which locates the reflector by correlating the forward source wavefield...
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Journal Article
Journal: The Leading Edge
Published: 01 November 2016
The Leading Edge (2016) 35 (11): 968–976.
...-principle , accessed 6 October 2016. Claerbout J. F. , 2005 , Basic Earth Imaging : Stanford Exploration Project . Colombo D. , and De Stefano M. , 2007 , Geophysical modeling via simultaneous joint inversion of seismic, gravity and electromagnetic data: Application to prestack...
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Journal Article
Journal: Geophysics
Published: 01 January 2000
Geophysics (2000) 65 (3): 861–873.
... ( Aki and Richards, 1980 ), (10) Substituting equation ( 8 ) for γ ib ( x b | x s ) and ∂ q s γ ib ( x b | x s ) in equation ( 9 ), the reconstructed Green's tensor at the new datum can be written (11) where V M,D ij and U M,D ij are given in Appendix...
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Journal Article
Journal: Geophysics
Published: 05 September 2006
Geophysics (2006) 71 (5): S185–S197.
... principle is mainly attributable to Claerbout (1971) . To compute the image at a point, we take the value at the point and time t = 0 of the crosscorrelation between the downgoing source wavefield and the upgoing data wavefield. The imaging principle used in the S-G implementation differs...
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Journal Article
Journal: Geophysics
Published: 01 January 2003
Geophysics (2003) 68 (2): 733–744.
... artifacts ( Gardner and Canning, 1994 ), prepare the data for wave-equation common-azimuth imaging ( Biondi and Palacharla, 1996 ), or provide the spatial coverage required for 3D multiple elimination ( van Dedem and Verschuur, 1998 ). Claerbout (1992 , 2003 ) formulated the general principle...
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Journal Article
Journal: Geophysics
Published: 17 August 2006
Geophysics (2006) 71 (4): SI221–SI229.
... ). The second step of shot-profile migration forms a subsurface image by an interferometric extraction of energy from the extrapola-ted source and receiver wavefields. Claerbout's imaging principle ( Claerbout, 1971 ) asserts that energy in the receiver wavefield R , spatially colocated with energy...
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