共接收点倾斜叠加波动方程偏移，本质上是一种叠前偏移方法。
Wave equation migration after common receiving point slant stacks (WEMCRPSS) is essentially a prestack migration method.
新的偏移算法考虑了倾斜的正交晶系各向异性，这对增强采样有一定的影响。
New migration algorithms incorporated tilted orthorhombic anisotropy, which leveraged the enhanced sampling.
该技术是将动校正后的数据偏移到倾斜反射界面零偏移距位置上，能够解决深层构造成像问题。
The normai moveout corrected seismic data are mi-grated to the zero offset dipping reflector, which solves the problem in deep layer image.
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