In seismic data processing, the commonly used R ado n transformation has linear R ado n transformation and parabolic R ado n transformation. Linear R ado n transformation, or S 2 p transformation, or slant stack, which is the data along a series of gradient t = S+ p x were overlapping, S to intercept time, p for ray parameters, classics After positive transformation, linear phase axis x 2 t domain, reflected in the form of hyperbolic in phase axis respectively mapped into S 2 p points and elliptic domain

线性 、 抛物 R ado n 变换的实现.txt

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