--> Estimation of Migration Velocity by Forward Modelling of Old Seismic Stacks
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Estimation of Migration Velocity by Forward Modelling of Old Previous HitSeismicNext Hit Stacks

Abstract

This research is a case study of southern basin in Iran where velocity modelling has been done on Asmari and Gachsaran formations. Geologically complex formations, it is important to determine the optimum velocity to achieve the best migratd Previous HitseismicNext Hit section. We introduced a method that the Previous HitseismicNext Hit processor can utilise to better migrate a post-stack Previous HitseismicNext Hit section. Methodology We have created a model by combining Previous HitinterpretationNext Hit of vintage Previous HitseismicNext Hit, surface geology and well Previous HitdataNext Hit (Fig. 1). Ray tracing was performed on the model with various velocity inputs. After each step, results analysed and the deviation from original horizons is estimated. The optimum velocity is the one that has the highest match with the input Previous HitdataNext Hit. The results of ray tracing will be sent back for re-Previous HitinterpretationNext Hit. The difference between the new Previous HitinterpretationNext Hit and the older one will hint on the corrections that need to be applied on the ray tracing model. Several methods are available for ray tracing. They vary in application based on the input Previous HitdataNext Hit. For this particular case, we have dealt with vintage stack Previous HitseismicNext Hit; hence vertical ray tracing has been used to achieve the optimum velocity of Previous HitdataNext Hit. Where there is mismatch between the model and the input Previous HitdataNext Hit, the amount and location of deviation will determine the appropriate adjustments for the next run. This iterative process will continue until the error falls below the defined threshold. Figure 2 illustrate deviation amount for two horizons. Conclusion This method will create a velocity file for post stack migration that can help checking processing steps as well as introducing some control on the Previous HitinterpretationNext Hit. Upon establishing an accurate velocity for each formation, analysis of rock properties and effects of changing in this parameter on wave propagation will be available with higher accuracy. With exported velocity file it will be possible to check other migration algorithm on Previous HitdataTop and make comparison between methods to achieve an acceptable migration of reflectors.