Creating a seismic image that is absolutely clear
 
 
     
 
 
 


  Saskatchewan, Canada

Data courtesy of Husky Energy Inc.

Event Similarity Prediction (ESP) enhances small and large scale structural and stratigraphic areas from seismic trace volumes. This process computes local trace-to-trace dissimilarity. The advantage of dissimilarity data is that it reveals and highlights lateral seismic changes that often relate to geologic changes. The dissimilarity measurements yield the visual identification of such features as faults, facies change and other geological patterns. Faults and stratigraphic changes will often stand out as prominent anomalies in otherwise homogeneous data.
 
        

 

   
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