论文部分内容阅读
The Z component and X component profiles of seismic waves extracted with the prestack Kirchhoff integral migration could approximate to the primary wave(P wave)and converted shear wave(PS wave)profiles under certain conditions.The relative change of their reflection amplitude reflects the formation stress anomaly and subsurface media anisotropy.The principle and method for extracting amplitude ratios were studied and the application of amplitude ratio profiles was also examined when processing and interpreting actual seismic data.The amplitude ratio profile is an effective supplementary means of identifying the stratigraphic boundary and lithology.
The Z component and X component profiles of seismic waves extracted with the prestack Kirchhoff integral migration could approximate to the primary wave (P wave) and converted shear wave (PS wave) profiles under certain conditions. The relative change of their reflection amplitude reflects the formation stress anomaly and subsurface media anisotropy. The principle and method for bedding ratio ratios was studied and the application of amplitude ratio profiles was also examined when processing and interpreting actual seismic data. amplitude ratio profile is an effective supplementary means of identifying the stratigraphic boundary and lithology.