Abstract:Rayleigh wave is a secondary wave characterized by low frequency and strong energy,propagating mainly along the interface of medium and rapid attenuation of energy with increase in interface distance. Like the reflection and refraction,the Rayleigh wave also contains geologic information of subsurface medium.Based on basic methods investigating near-surface structure by Raileigh wave,the paper computes near-surface structure using real data of multi-layers and dip-layers,which proved again that it is feasibility using Rayleigh wave on seismic single shot records for investigation of near-surface structure.
王振国, 周熙襄. 再论利用瑞利面波调查表层结构的可行性[J]. 石油地球物理勘探, 2004, 39(5): 505-508,538.
Wang Zhen-guo, Zhou Xi-xiang. Discussing again about possibility using Rayleigh wave for investigation of near-surface structure. OGP, 2004, 39(5): 505-508,538.