210 likes | 368 Views
VSP->SWP Interferometry. Redatum sources below overburden. Local VSP migration. 3x3 Classification Matrix. SSP. VSP. SWP. SSP. SSP. SSP. SSP. VSP. SSP. SWP. VSP. VSP. SSP. VSP. VSP. VSP. SWP. SSP. SWP. SWP. SWP. VSP. SWP. SWP. Motivation.
E N D
VSP->SWP Interferometry Redatum sources below overburden Local VSP migration
3x3 Classification Matrix SSP VSP SWP SSP SSP SSP SSP VSP SSP SWP VSP VSP SSP VSP VSP VSP SWP SSP SWP SWP SWP VSP SWP SWP
Motivation Problem: Overburden+statics defocus VSP migration Solution: VSP -> SWP Transform Redatum sources below overburden Local VSP migration
Outline • Motivation • Interferometry Theory • Numerical Examples • Conclusion
SWP VSP { { Im G(B|A) + S S 0 0 0 0 Reciprocity Correlation Equation Far-field VSP -> SWP Transform = kG(B|x)* G(A|x) S0 x S A 0 B
Outline • Motivation • Interferometry Theory • Numerical Examples: 3 Syn. Data • Conclusion
FD Experiment 1500 0 Depth (m) Time (s) Reflection wavefield 3500 3 Offset (m) 1000 Depth (m) 3500 0 1500
Reduced Form GSM Ray tracing of line source (picked direct wave) Reduce form GSM result 1500 ? Depth (m) 3500 0 Offset (m) 1000 0 Offset (m) 1000
Reduced Form GSM Ray tracing of line source (picked direct wave) Reduce form GSM result 1500 Lesson: Super-resolution ? Depth (m) 3500 0 Offset (m) 1000 0 Offset (m) 1000
Synthetic Experiment(He, 2006) 0 10 shots Depth (m) Overburden 94 geophones 5500 0 km 7 km Offset (m)
A Shot Gather 0 s 5 s 2 km 6.5 km
WEIM Result (one shot) 2700 Depth (m) Artifacts 5500 0 1700 Offset (m)
Tricks: Filter down and up going waves: m(x) = U(x)/D(x) Lesson: Fltering+extra stacking reduces artifacts WEIM Result (ten shots) 2700 Depth (m) 5500 0 1700 Offset (m)
Outline • Motivation • Interferometry Theory • Numerical Examples: GOM Data • Conclusion
120 shots ? 98 geophones Poor image of flank by standard migration VSP Salt Flank Imaging (BP Hornby et al, 2006) Overburden
VSP Data 3.2 s 0 2000 ft 7.2 s
Interferometric Migration Result 0 2000 ft
VSP->SWP Summary ! 1. Redatum sources below overburden 2. Local VSP migration 3. Kills Source Statics and no need to know src location or excitation time 4. Super-resolution 5. Instead of redatuming receivers to surface, we redatum sources to depth.
X (m) 1000 1400 950 Depth (m) 1950
Main Parameters in VSP: • Source number: 100 • Shot interval: 10 m • Receiver number: 91 • Receiver interval: 10 m • Depth of the first receiver: 950 m • Depth of the last receiver: 1850 m • Temporal interval: 0.001 s