叠加地震数据是作为简单界面和薄层反射的叠加而被模拟的。这种参数化过程允许采用一个省时的块状阻抗模型。该方法是用来替代典型的最小均方差方法,实质上类似于最小熵反褶积和稀疏脉冲反演,尽管在实现的过程中,较为简单,且也有许多的不同 Overlapped seismic data was modeled as a superposition of simple and thin-layer reflections. This parameterization allows the use of a time-saving bulk impedance model. This method is used to replace the typical minimum mean square error method, which is essentially similar to minimum entropy deconvolution and sparse pulse inversion, though it is simpler in implementation and has many differences