Download - Adaptive Grid Reverse-Time Migration
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Adaptive Grid Adaptive Grid Reverse-Time MigrationReverse-Time Migration
Yue WangYue Wang
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OutlineOutline
• Motivation and ObjectiveMotivation and Objective
• Reverse Time MethodologyReverse Time Methodology
• Salt Dome Model TestSalt Dome Model Test
• Field Data TestField Data Test
• ConclusionsConclusions
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ProblemProblem
• Kirchhoff migration is not Kirchhoff migration is not optimal for complex velocity optimal for complex velocity model.model.
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Marmousi ModelMarmousi Model
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
33
00
00 99
Low-velocity wedgeLow-velocity wedge
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ProblemProblem
Using first arrival time Using first arrival time
Difficulty in imagingDifficulty in imaging
Kirchhoff migrationKirchhoff migration
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ProblemProblem
Reverse-Time Migration RTM) Reverse-Time Migration RTM)
Image complex structure Image complex structure ExpensiveExpensive
Using multi-arrival time Using multi-arrival time
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SolutionSolution
Fast RTM Fast RTM
Variable grid size Variable grid size Variable time step Variable time step
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ObjectiveObjective
• Develop fast reverse time migration for Develop fast reverse time migration for land and marine multi-component dataland and marine multi-component data
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OutlineOutline
• Motivation and ObjectiveMotivation and Objective
• Reverse Time MethodologyReverse Time Methodology
• Salt Dome Model TestSalt Dome Model Test
• Field Data TestField Data Test
• ConclusionsConclusions
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Reverse Time OperatorReverse Time Operator
Elastic wave equationElastic wave equation
A 2-4 staggered-grid FD solverA 2-4 staggered-grid FD solver
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Variable Grid SizeVariable Grid Size
DistanceDistance
Dep
thD
epth
Low velocity Low velocity
High velocity High velocity
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Variable Grid SizeVariable Grid Size
Fine grid (dx dz)Fine grid (dx dz)
Coarse grid (3dx 3dz)Coarse grid (3dx 3dz)
zz
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Variable Grid SizeVariable Grid Size
Use wave equation to Use wave equation to propagate wavespropagate waves
Fine gridFine grid
Coarse gridCoarse grid
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Variable Time StepVariable Time Step
coarse grid, fine time stepcoarse grid, fine time step
coarse grid, coarse time stepcoarse grid, coarse time step
DistanceDistance
Dep
thD
epth
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Variable Time StepVariable Time Step
zz
dtdt
tt
dtdt
3 dt3 dt
dtdt
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Variable Time StepVariable Time Step
zz
Fine time stepFine time step
Coarse time stepCoarse time step
tt
Use wave equation to Use wave equation to propagate wavespropagate waves
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Variable Time StepVariable Time Step
Falk et al. (1998, Geophys. Pros. ):Falk et al. (1998, Geophys. Pros. ):
1. Non-staggered-grid FD1. Non-staggered-grid FD
2. 2x time step change2. 2x time step change
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Variable Time StepVariable Time Step
The new method :The new method :
1. Staggered-grid FD1. Staggered-grid FD
2. 3x time step change2. 3x time step change
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Numerical ResultsNumerical Results
Fine time stepFine time step
Time t1Time t1
Am
pli
tud
eA
mp
litu
de
Coarse time step Coarse time step DepthDepth
DepthDepth
Time t2Time t2
Am
pli
tud
eA
mp
litu
de
No artificial reflectionsNo artificial reflections
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OutlineOutline
• Motivation and ObjectiveMotivation and Objective
• Reverse Time MethodologyReverse Time Methodology
• Salt Dome Model TestSalt Dome Model Test
• Field Data TestField Data Test
• ConclusionsConclusions
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Salt ModelSalt Model
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
2.72.7
00
00 4.54.5
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Velocity ProfileVelocity Profile
Velocity (km/s)Velocity (km/s)
Dep
th (
km
)D
epth
(k
m)
Velocity (km/s)Velocity (km/s)1.51.5 44 00 222.72.7
00
Dep
th (
km
)D
epth
(k
m)
2.72.7
00
PP SS
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Velocity ProfileVelocity Profile
Velocity (km/s)Velocity (km/s)
Dep
th (
km
)D
epth
(k
m)
Velocity (km/s)Velocity (km/s)1.51.5 44 00 222.72.7
00
PP SSFine grid sizeFine grid sizeFine time stepFine time step
Coarse grid sizeCoarse grid sizeCoarse time stepCoarse time step
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Shot GatherShot GatherNormal StressNormal StressVerticalVerticalHorizontalHorizontal
Tim
e (s
) T
ime
(s)
Distance (km)Distance (km)22
00
0.90.9 3.63.6 Distance (km)Distance (km)0.90.9 3.63.6 Distance (km)Distance (km)0.90.9 3.63.6
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Kirchhoff MigrationKirchhoff Migration
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
2.52.5
00
0.450.45 4.054.05
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Kirchhoff MigrationKirchhoff Migration
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
2.52.5
00
0.450.45 4.054.05
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Reverse Time MigrationReverse Time Migration
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
2.52.5
00
0.450.45 4.054.05
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Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
2.52.5
00
0.450.45 4.054.05
Reverse Time MigrationReverse Time Migration
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OutlineOutline
• Motivation and ObjectiveMotivation and Objective
• Reverse Time MethodologyReverse Time Methodology
• Salt Dome Model TestSalt Dome Model Test
• Field Data TestField Data Test
• ConclusionsConclusions
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Processed CSGProcessed CSG
2.72.7
00Radial Component Radial Component Vertical Component Vertical Component
Tim
e (s
) T
ime
(s)
Trace NumberTrace Number Trace NumberTrace Number00 8080 00 8080
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Common Offset GatherCommon Offset Gather((Vertical Component)Vertical Component)
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727
Signal/Noise Ratio HighSignal/Noise Ratio High
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Common Offset GatherCommon Offset Gather((Radial Component)Radial Component)
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727
Signal/Noise Ratio LowSignal/Noise Ratio Low
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Kirchhoff MigrationKirchhoff Migration((Vertical Component)Vertical Component)
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727
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Kirchhoff MigrationKirchhoff Migration((Radial Component)Radial Component)
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727
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RTMRTM
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727
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Comparison Comparison
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
44
00
00 2727Distance (km)Distance (km)00 2727
RTMRTM KMKM
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OutlineOutline
• Motivation and ObjectiveMotivation and Objective
• Reverse Time MethodologyReverse Time Methodology
• Salt Dome Model TestSalt Dome Model Test
• Field Data TestField Data Test
• Conclusions and Future WorkConclusions and Future Work
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ConclusionsConclusions
• Variable RTM Variable RTM 10 times faster10 times faster than standard RTM than standard RTM• Migrates Land and marine multi-component dataMigrates Land and marine multi-component data• Use primary and multiple reflections for imagingUse primary and multiple reflections for imaging
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AcknowledgementAcknowledgement
We are grateful to the 1999 sponsors We are grateful to the 1999 sponsors of the UTAM consortium for the of the UTAM consortium for the financial supportfinancial support
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Raw CSGRaw CSGT
ime
(s)
Tim
e (s
)
2.72.7
00Radial Component Radial Component Vertical Component Vertical Component
00 8080 00 8080Trace NumberTrace Number Trace NumberTrace Number
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Main Processing FlowMain Processing FlowGeometry assignment, datuming and so on
Trace editing
Surface wave attenuation, amplitude balancing
P-velocity analysis
S-velocity analysis
Relative gain compensation, surface velocity estimation
KM RTM
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Shallow VelocityShallow Velocity
Distance (km)Distance (km)
Dep
th (
km
)D
epth
(k
m)
0.40.4
00
00 2727
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Future WorkFuture Work
• Apply the RTM scheme for data set with Apply the RTM scheme for data set with more complex structures.more complex structures.