稀疏脉冲反褶积是一种从地震记录中估计振幅和位置的反演方法。-Sparse deconvolution is a pulse inversion method estimates the amplitude and position seismic records.

最小平方反褶积是把地震子波压缩成尖脉冲，从而使地震记录能够直接反映地下反射系数序列-Least squares deconvolution of seismic waves are compressed into spikes, which can directly reflect the seismic record subsurface reflection coefficient series

子波整形反褶积是通过所设计的整形滤波器对地震子波，使其成为所期望的形状。-Shaping wavelet deconvolution by shaping filter designed for seismic waves, making it the desired shape.

有限差分正演模拟，进行地震波正演，源码是科罗拉多矿业学院开发的。-Finite difference forward modeling for seismic wave forward modeling, the code is the Colorado school of mining .