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- W2101472629 abstract "In recent papers, Taner et al. (1970) and Schneider (1971) pointed out that when the subsurface varies laterally at a rate such that all rays collected for velocity analysis do not penetrate the same earth column, the velocity found from the analysis will be erroneous. The conclusions of Taner were based on ray‐tracing computations; Schneider did not state the basis for his illustrations. If we are willing to assume the Dix (1955) approximation, i.e., that a time‐distance curve for a reflection from a plane is the hyperbola [Formula: see text] we can predict, at least roughly, the magnitude of the errors discussed by Taner and Schneider. In equation (1), t is traveltime for a reflection detected by a geophone a distance X from the source. [Formula: see text] is the traveltime for X = 0 and V is the rms velocity (see Dix)." @default.
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- W2101472629 date "1973-08-01" @default.
- W2101472629 modified "2023-10-14" @default.
- W2101472629 title "THE EFFECT OF LATERAL INHOMOGENEITY ON VELOCITY DETERMINATION" @default.
- W2101472629 cites W1984898923 @default.
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- W2101472629 doi "https://doi.org/10.1190/1.1440374" @default.
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