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Imaging Multiple Reflections with Reverse- Time Migration Yue Wang University of Utah
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Outline BackgroundBackground Motivation & ObjectiveMotivation & Objective MethodologyMethodology Numerical ExamplesNumerical Examples ConclusionsConclusions
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Forward Process Distance (km) Depth (km) 1 0 04.5 * Source Geophone Line
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Forward Process Distance (km) Depth (km) 1 0 04.5 * obs
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Reverse Time Migration Distance (km) Depth (km) 1 0 04.5 obs Extrapolated Wavefield obs Reversed traces
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Reverse-Time Migration Extrapolated Wavefield Imaging Condition Migration Section
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Outline BackgroundBackground Motivation & ObjectiveMotivation & Objective MethodologyMethodology Numerical ExamplesNumerical Examples ConclusionsConclusions
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Ocean-Bottom Survey Distance (km) Depth (km) 1 0 04.5 * Source Geophone Line
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Problem Distance (km) Depth (km) 1 0 04.5 * Receiver-side Multiples
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Synthetic Shot Gather Time (s) Distance (km) Receiver side multiples 2 0 0.93.6
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Field Data Time (s) Distance (m) 4 0 -80 1900 Receiver side multiples
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Time Migration Time (s) Distance (m) 4 0 -80 1900 Receiver side multiples
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Objective Using both primary and multiple reflections for imaging by reverse- time migration.Using both primary and multiple reflections for imaging by reverse- time migration.
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Outline BackgroundBackground Motivation & ObjectiveMotivation & Objective MethodologyMethodology Numerical ExamplesNumerical Examples ConclusionsConclusions
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Ocean-Bottom Survey Distance (km) Depth (km) 1 0 04.5 * Source Geophone Line
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Ocean-Bottom Survey Distance (km) Depth (km) 1 0 0 *PV Up-going
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Multi-Component Data pressure + particle velocity ( P & V ) ocean-bottom survey
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Reverse Time Migration Distance (km) Depth (km) 1 0 0PV Down-going PV ( P & V Scheme )
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Reverse Time Migration Distance (km) Depth (km) 1 0 0VV ( Particle Velocity Only )
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Key Idea Primary + Multiple Correct Positions P & V Scheme
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Key Idea Primary + Multiple Incorrect Positions V-Only Scheme
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Ocean-Bottom Survey Distance (km) Depth (km) 1 0 0 *PV Up-going Waves
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P & V Scheme Distance (km) Depth (km) 1 0 0PVPV Correct Position Down-going waves
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Particle Velocity Only Scheme Distance (km) Depth (km) 1 0 0VV Incorrect
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Ocean-Bottom Survey Distance (km) Depth (km) 1 0 0 *PV Down-going waves ( Multiples )
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P & V Scheme Distance (km) Depth (km) 1 0 0PVPV Correct Position Up-going waves
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Particle Velocity Only Scheme Distance (km) Depth (km) 1 0 0VV Incorrect
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Outline BackgroundBackground Motivation & ObjectiveMotivation & Objective MethodologyMethodology Numerical ExamplesNumerical Examples Salt Dome Model Salt Dome Model ConclusionsConclusions
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Salt Model Distance (km) Depth (km) 2.7 0 04.5
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Shot Gather Normal Stress VerticalHorizontal Time (s) Distance (km) 2 0 0.93.6 0.93.6 0.93.6 Multiples
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Kirchhoff Migration Distance (km) Depth (km) 2.5 0 0.454.05
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Kirchhoff Migration Distance (km) Depth (km) 2.5 0 0.454.05
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Particle Velocity Only Scheme Distance (km) Depth (km) 2.7 0 0.454.05
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Particle Velocity Only Scheme Distance (km) Depth (km) 2.7 0 0.454.05
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P & V Scheme Distance (km) Depth (km) 2.5 0 0.454.05
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Distance (km) Depth (km) 2.5 0 0.454.05 P & V Scheme
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Primary + Multiple Correct Positions Conclusion P + V RTM
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Future Work: Field Data Test Time (s) Distance (m) 40-80 1900 Receiver side multiples
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Acknowledgement We are grateful to the 1999 sponsors of the UTAM consortium for the financial support
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Outline BackgroundBackground Motivation & ObjectiveMotivation & Objective MethodologyMethodology Numerical ExamplesNumerical Examples Plane-wave example Plane-wave example ConclusionsConclusions
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Forward Process Distance Depth Up-going waves
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P & V Scheme Distance Depth Down-going waves
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P & V Scheme Time (s) Depth (km) 0 0.8 0 1.2 Down-going waves
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Particle Velocity Only Scheme Distance Depth Down-going waves Up-going waves
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Particle Velocity Only Scheme Time (s) Depth (km) 0 0.8 0 1.2 Down-going waves Up-going waves
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P + V RTM Distance (km) Depth (km) 100 P+V Up-going waves Correct Position Distance (km) Depth (km) 1 0 0 P Down-going waves Up-going waves
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