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利用CDP资料能够模拟出平面波前地震剖面,它比直接由野外获得的平面波前记录优越得多。平面波前法地震剖面既可以用来研究地质构造形态,又可用来进行地震地层学的研究,它可以作为常规地震方法的补充。
Using CDP data it is possible to simulate a planar wavefront seismic profile that is much superior to the planar wavefront records obtained directly in the field. The plane wave front seismic section can be used not only to study the geological structure, but also to study the seismic stratigraphy. It can be used as a supplement to conventional seismic methods.