Advanced Seismic ImagingAdvanced Seismic ImagingGG 6770GG 6770
Variance Analysis of Seismic Variance Analysis of Seismic Refraction Tomography DataRefraction Tomography Data
ByByTravis CrosbyTravis Crosby
Outline
• Description of field experimentDescription of field experiment
• Description of refraction tomography processing Description of refraction tomography processing and inversionand inversion
• Description of variance analysisDescription of variance analysis
• Results of tomography experimentResults of tomography experiment
• Results of variance analysisResults of variance analysis
Seismic Data Acquisition Parameters
GeophonesGeophones - 120 40-Hz vertical component at 5 meter intervals.
SourceSource - Elastic Weight Drop with 550 pound hammer activated at 20 meter intervals (every 4th geophone). 31 total shot points per line. Five impacts summed per shot point.
RecordingRecording - 0.5 ms sample rate, 2000 samples per trace, 1 second listening time.
Seismic Data Processing Parameters
- 3188 traveltimes picked (out of 3720 total)
- 0.6 meter grid size
- One dynamic smoothing schedule 21x11 30 iterations
- 3.9 times more knowns (traveltimes) than unknowns (smoothing schedule)
- Final residual 3.9 ms
Residual vs Iteration
Description of Variance Analysis
- Velocity data was obtained from 30 inversions where first-arrival time was randomly altered up to ± 4 ms ( ¼ period of average first arrival).
- The sample variance of each slowness cell over the 30 samples was determined.
- The variance provides an idea of how widely spread the values of each slowness cell are likely to be.
- The larger the variance, the more scattered the velocities are. It may be inferred that there is more uncertainty in these parts of the model.
- Sample variance:S² = Σ (xi – xave)² / n-1