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

Migration with CRS   Please note the great improvements in the data quality, especially in the low fold areas.   For more information about the technology or for testing purposes, please contact us at: info@guidegeoscience.com

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