Common Reflection Surface (CRS)
Common Reflection Surface
Processing provides tools for bringing structural
information into time processing. This structure can be used
for data enhancement, velocity analysis, or even residual
move-out analysis.
Improves seismic data in thrust-belt regimes and complex
geological settings such as in sub-salt areas.
Improves fault definition especially around severe
shadow zones.
Enhances deep data with no lateral smoothing but based
on semblance analysis within the Fresnel Zone.
Migration without CRS
