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在处理多种震源联合激发地震资料时，首先要解决不同种震源地震记录子波的相位差异和振幅差异。消除地震记录子波的相位差异是通过优化模型道和对反褶积前的地震记录子波做最小相位化来实现的。消除振幅差异则通过优化频率范围、地表一致性反褶积以及谱均衡来解决。通过二维、三维实际资料处理表明，本文所介绍的处理方法是可行的。
When dealing with seismic data from a variety of sources, we must first solve the phase difference and amplitude difference of seismograms from different kinds of sources. Eliminating the phase difference of the seismogram wavelet is achieved by optimizing the model tract and minimizing the phase of the seismogram wavelet before deconvolution. The elimination of amplitude differences is addressed by optimizing the frequency range, surface-consistent deconvolution, and spectral equalization. Through two-dimensional, three-dimensional actual data processing shows that the method described in this article is feasible.