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Least-squares Joint Imaging of Primaries and Multiples
Morgan Brown Stanford University 2002 SEG, Salt Lake City Stanford Exploration Project Brown
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A Stack of the Primaries...
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…and a Stack of the Multiples
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CMP gathers are also consistent
primaries multiples Stanford Exploration Project Brown
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What information can multiples add?
At least redundant: Related AVO behavior Similar structural image Different illumination: Near offsets Shadow zones Stanford Exploration Project Brown
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How to exploit the information?
Constraint on existing information Integrate additional information Three requirements: Image self-consistency Consistency with data Simplicity of images Stanford Exploration Project Brown
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The Gameplan Imaging: “NMO for Multiples” Constraint/Integration:
Regularized least-squares inversion Synthetic & Real data tests Stanford Exploration Project Brown
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NMO for multiples - kinematics
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NMO for multiples - kinematics
Building a pseudo-primary t’ S R 1 t’ t Stanford Exploration Project Brown
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NMO for multiples - kinematics
Building a pseudo-primary t’ S R 2 t’ t Stanford Exploration Project Brown
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NMO for multiples - kinematics
Building a pseudo-primary t’ S R 3 t’ t Stanford Exploration Project Brown
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NMO for multiples - kinematics
Building a pseudo-primary t’ S R 4 t’ t Stanford Exploration Project Brown
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NMO for multiples - kinematics
Building a pseudo-primary t’ S R t’ t Dx Stanford Exploration Project Brown
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NMO for multiples - kinematics
primary NMO for multiple 1 Effective RMS velocity Stanford Exploration Project Brown
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NMO for multiples - kinematics
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Modeling Amplitudes: Assumptions
Constant AVO WB reflection. Free surface R.C. = -1. Ignore geometric spreading. Ignoring primary AVO: multi (-r)i*prim AVO: more later. Stanford Exploration Project Brown
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Forward Modeling Equation
NMO0 d m0 Stanford Exploration Project Brown
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Forward Modeling Equation
(-r)*NMO1 d m1 Stanford Exploration Project Brown
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Forward Modeling Equation
(-r)2*NMO2 d m2 Stanford Exploration Project Brown
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Forward Modeling Equation
Ni :adjoint of NMO for multiple i. Ri : (-r)iI. mi : pseudo-primary panel i. d : input CMP gather. Stanford Exploration Project Brown
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Least-squares objective function
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Least-squares objective function
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Image Simplicity and Crosstalk
Ideally, the “simplest” model... N0m0 + N1R1m1 + N2R2m2 “inverse” d m0 m1 m2 Stanford Exploration Project Brown
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Model Simplicity and Crosstalk
…but this problem is underdetermined. N0m0 + N1R1m1 + N2R2m2 “inverse” d m0 m1 m2 Stanford Exploration Project Brown
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Discriminating between crosstalk and signal
Self-consistent, flat primaries Stanford Exploration Project Brown
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Discriminating between crosstalk and signal
Inconsistent, curved crosstalk Stanford Exploration Project Brown
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Model Regularization suppresses crosstalk
Dm= Difference between pseudo-primary panels. Penalizes inconsistent crosstalk events. Dx= Difference along offset. Penalizes curving events. e1,e2 = Scalar regularization parameters. Stanford Exploration Project Brown
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Dm: Modeling AVO of multiples
No explicit AVO modeling Model relative primary/multiple AVO dependence. Dm differences at different offsets. Stanford Exploration Project Brown
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Dm: Modeling AVO of multiples
From forward model Mult(h) ~ prim(hp) * (-r) hp S R t’ h t Stanford Exploration Project Brown
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Dm: Modeling AVO of multiples
In constant velocity: hp S R t’ h t Stanford Exploration Project Brown
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Dm: Modeling AVO of multiples
In constant velocity: Curves: hp(t) - - m0 m1 Stanford Exploration Project Brown
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Synthetic Data Results
Raw primaries Raw mult. 1 Raw mult. 2 Stanford Exploration Project Brown
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Synthetic Data Results
Est. primaries Est. mult. 1 Est. mult. 2 x(-r) x(-r 2) Stanford Exploration Project Brown
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Synthetic Data Results
Raw primaries Est. primaries Difference Stanford Exploration Project Brown
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Synthetic Data #2 Results
Raw primaries Est. primaries Difference Stanford Exploration Project Brown
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Real Data Results Raw primaries Est. primaries Difference
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Strengths Good separation…. Amplitude-preserving process
...at near offsets …without a prior noise model Amplitude-preserving process General integration framework Stanford Exploration Project Brown
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Weaknesses 1-D earth. Amplitudes - Incomplete Modeling?
Parameter sensitivity… …e1, e2, r, velocity. Multiples coherent across offset. NMO stretch. Stanford Exploration Project Brown
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The Future Migration…tougher battle, richer spoils
Different illumination Amplitudes? Converted waves (PS,PSP). “Tall” operator. One image, many datasets. Prior wavefield separation. Stanford Exploration Project Brown
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Acknowledgements ExxonMobil, WesternGeco for data.
Biondo Biondi, Bob Clapp, Antoine Guitton. Stanford Exploration Project Brown
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