1887

Abstract

More than the absorption in the earth layers, the processing, and more precisely the NMO correction, are responsible for the attenuation of high frequenties in seismic sections . Any improvement in the high-frequency content of the stacked sections and in the determination of the interval velocities implies, for modeling the NMO curve of the recorded reflections, a mathematical expression

/content/papers/10.3997/2214-4609.201410503
1992-06-01
2021-04-17