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Arbitrary Parameter Extraction, Stationary Phase Migration, and Tomographic Velocity Analysis. Jing Chen University of Utah. Outline. Parameter Extraction Stationary Phase Migration Tomographic Velocity Analysis Conclusions. Parameter Extraction.
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Arbitrary Parameter Extraction, Stationary Phase Migration, and Tomographic Velocity Analysis Jing Chen University of Utah
Outline • Parameter Extraction • Stationary Phase Migration • Tomographic Velocity Analysis • Conclusions
Parameter Extraction Extract specular-ray related parameters from prestack migration S G R
Why Specular-Ray Parameters Needed ? • Prestack Depth Migration • Traveltime Inversion • Tomographic MVA • AVO • Etc...
Prestack Migration Operator Image Aperture Weight Data
Weighted Prestack Migration Operator Image Aperture Weight Data Parameter
R Specular-Ray Related Parameters Source Receiver Midpoint Traveltime Reflector Normal Departure Angle Emergence Angle Incidence Angle
Parameter Extraction Synthetic Data Examples: Migrate a COG; Extract Midpoint Coordinates, Traveltimes, and Incidence Angles.
Distance (km) 0 4 8 12 16 0 1 Depth (km) 2 3 4 Kirchhoff Migration of a COG
Distance (km) 0 4 8 12 16 0 1 Depth (km) 2 3 4 Weighted Kirchhoff Migration of a COG Extra Weight
COG Incidence Angles Distance (km) 0 8 16 0 20 (Degrees) Depth (km) 10 2 4 0
COG Incidence Angles Distance (km) 0 8 16 0 20 (Degrees) Depth (km) 10 2 4 0
COG Traveltimes Distance (km) 0 8 16 3.5 0 (Seconds) Depth (km) 1.75 2 4 0
COG Traveltimes Distance (km) 0 8 16 3.5 0 (Seconds) Depth (km) 1.75 2 4 0
COG S-R Midpoint Coordinates Distance (km) 0 8 16 20 0 Depth (km) (km) 10 2 4 0
COG S-R Midpoint Coordinates Distance (km) 0 8 16 20 0 Depth (km) (km) 10 2 4 0
Distance (km) 0 4 8 12 16 0 1 Depth (km) 2 3 4 Verification of Extracted Parameters
COG S-R Midpoint Coordinates Distance (km) 0 8 16 20 0 Depth (km) (km) 10 2 4 0
COG Traveltimes Distance (km) 0 8 16 3.5 0 (Seconds) Depth (km) 1.75 2 4 0
Verification of Extracted Parameters Trace Midpoint Coordinates 11 13 15 1 Time (sec) Trvaeltimes Extracted 2
Applications • Stationary Phase Migration • Tomographic Velocity Analysis
Stationary Phase Migration SPM uses specular-ray parameters to : • Migrate traces within Fresnel zone • Reject traces out of Fresnel zone • Suppress alias artifacts
Stationary Phase Migration • Algorithm • Synthetic Data Example • Field Data Example
Stationary Phase Migration Operator Schleicher et al. (1997) : Fresnel zone width Minimum Aperture Fresnel Zone Stationary phase point
Stationary Phase Migration • Algorithm • Synthetic Data Example • Field Data Example
Kirchhoff Migration of a COG Distance (km) 0 4 8 12 16 0 1 2 Depth (km) 3 4
Stationary Phase Mig. of a COG Distance (km) 0 4 8 12 16 0 1 2 Depth (km) 3 4
Migration Operator Trace Contributions
Trace Contributions : KM Trace Number 0 150 300 0 Depth (km) 2 4
Trace Contributions : SPM Trace Number 0 150 300 0 Depth (km) 2 4
Trace Contributions : KM Trace Number 0 150 300 0 Depth (km) 2 4
Trace Contributions : SPM Trace Number 0 150 300 0 Depth (km) 2 4
Trace Contributions : KM Trace Number 0 150 300 0 Depth (km) 2 4
Trace Contributions : SPM Trace Number 0 150 300 0 Depth (km) 2 4
Incidence Angle CIG Offset (km) Offset (km) 0 3 0 3 0 70 0 Depth (km) Depth (km) 35 2 2 4 4 0 (Deg)
Incidence Angle CIG Offset (km) Offset (km) 0 3 0 3 0 70 0 Depth (km) Depth (km) 35 2 2 4 4 0 (Deg)
Stacked SPM Image After Muting Distance (km) 0 4 8 12 16 0 1 2 Depth (km) 3 4
Stacked SPM Image Without Muting Distance (km) 0 4 8 12 16 0 1 2 Depth (km) 3 4
Stationary Phase Migration • Algorithm • Synthetic Data Example • Field Data Example
Kirchhoff Migration of a COG Distance (km) 0 2 4 6 8 10 12 14 0 2 Depth (km) 4 6
Stationary Phase Mig. of a COG Distance (km) 0 2 4 6 8 10 12 14 0 2 Depth (km) 4 6
Stacked KM Image Distance (km) 0 2 4 6 8 10 12 14 0 2 Depth (km) 4 6
Stacked SPM Image Distance (km) 0 2 4 6 8 10 12 14 0 2 Depth (km) 4 6
Stationary Phase Mig. vs Wavepath Mig. S G • Both approaches suppress alias artifacts • WM measures emergence angles in the data domain • SPM extracts parameters in the migration domain • SPM extracts more parameters • WM is faster • SPM may be more robust in parameter estimations
Applications • Stationary Phase Migration • Tomographic Velocity Analysis
Steps in Tomographic MVA • Build up Initial Migration Velocity • Migrate Seismic Data • Obtain S & R Coordinates • Find Specular-Ray Paths • Pick Depth Residual Moveouts • Pick Reflector Positions • Update Velocities • Migrate Seismic Data With • Updated Velocities • Repeat Above Steps