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- W2372187532 abstract "The conventional static correction method is characterized by vertical time migration and following static correction processing the reflection time for all of seismic traces could give rise to the same time-migration responses from the shallow to deep strata. Such a variation at tO occurred in static correction that could not change the patterns of reflection events might allow the relevant dynamic correction velocity (normally called stack velocity) to be changed. This variation of stack velocity generally depends on variation of the static correction on reflected tO that tends to being related to selection of datum level available for static correction and base level for seismic data processing. In the relatively ordinary area of subsurface structure, it is closer between the derived stack velocity and observed apparent velocity of seismic reflection event; but in the complicated area of subsurface structure and relief region, there exist very obvious influences of the static correction velocity on the dynamic correction velocity following datum static correction and particularly regional static correction, hence, if the latter (stack velocity) is applied for structural and geologic interpretations, greater errors will take place in this case. This paper makes a quantitative analysis of the influence of static correction on seismic velocity field based on above results from theoretical model study, and provides sound theoretical bases for the datum determination and application of the datum static correction in future." @default.
- W2372187532 created "2016-06-24" @default.
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- W2372187532 date "2004-01-01" @default.
- W2372187532 modified "2023-09-27" @default.
- W2372187532 title "Effect of Static Correction on Stack Velocity in Seismic Data Processing" @default.
- W2372187532 hasPublicationYear "2004" @default.
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