在地震数据处理中, 常用的 R ado n 变换有线性 R ado n 变换和抛物 R ado n 变换 。 线性 R ado n 变换, 或

S 2 p 变换, 或倾斜叠加, 是将数据沿着一系列倾斜线 t= S + p x 进行叠加, S 为截距时间, p 为射线参数, 经

过正变换后, x 2 t 域的线性同相轴 、 双曲线形态的反射同相轴分别被映射为 S 2 p 域的点和椭圆-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