将标准褶积模型推广后,我们可行及炮点及检波点移动对地震数据的影响。尤需注意的是,检波点移动将引入时变空间时移,同时,炮点移动将使单道时间褶积震源信号的影响转换为多道时空褶积。这些结果与经典多普勒理论是一致的。其意义在于,即使采用较低的采集速度,多普勒时移也将给地震数据带来误差。业已证明,在海上可控震源采集过程 After the general convolution model is generalized, we can do some researches on the seismic data affected by the movement of shot and detection points. It should be noted that the movement of detection point will introduce the time-varying space-time shift. Meanwhile, the movement of the shot point will transform the influence of single-channel time convoluted source signal into multi-channel temporal convolution. These results are consistent with the classical Doppler theory. The significance of this is that Doppler shift will bring errors to the seismic data, even at lower acquisition speeds. It has been proven that the acquisition of vibroseis at sea