变参考慢度Rytov近似傅氏偏移方法

针对常规Rytov近似傅氏偏移方法对于剧烈横向变速介质不能精确成像的状况,提出了变参考慢度Rytov近似傅氏偏移方法,从理论上解决了任意速度变化地质模型的偏移成像问题。为了进一步提高复杂地层的成像精度和波场延拓算子的稳定性,对散射波场的计算公式作了改进。将该方法运用于盐丘模型的正演和偏移试验,与常规Rytov近似偏移方法相比较可明显看出,变参考慢度Rytov近似傅氏偏移方法的处理效果得到了改善,其处理横向速度变化的能力大大增强。

Rytov approximation Fourier migration method with variable reference slowness

Because the conventional Rytov approximation Fourier migration method cannot accurately image the media with acute lateral variation of velocity, a Rytov approximation Fourier migration method with variable reference slowness was proposed to theoretically solve the migration image of the arbitrary velocity change model. In order to raise the imaging accuracy of complex layer and the stability of wavefield continuation operator, the scattered wavefield formula was improved. This method was applied to the foreword modeling and migration test of salt body model. The results show that Rytov approximation Fourier migration method with variable reference slowness is more efficient than the conventional Rytov approximation migration method. The ability for processing the variation of the lateral velocity increases greatly.