Abstract
AbstractCommon midpoint data are now being collected with ever increasing source‐receiver offsets. For wide aperture seismic data classical methods of interpretation fail, since velocity analyses and signal‐to‐noise enhancement methods based on hyperbolic traveltime curves are no longer appropriate. Therefore, the goals of increased velocity resolution and signal enhancement, which motivate the increase in offset, are not achieved. Approximate methods, involving higher order traveltime curves or extrapolations, have been developed for velocity analysis but these are ineffective in the presence of refracted arrivals, and lack a physical basis. These problems can be minimized by transforming the observational data to the domain of intercept or vertical delay time τ and horizontal ray parameter p. In this domain headwave refractions are collapsed into points and both near vertical and wide angle reflections can be analyzed simultaneously to derive velocity‐depth information, even in the presence of velocity gradients or low velocity zones.
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