应用此方法不仅避免了单井分层主观随意性，又对现场层位追踪起到了一定的指导作用。
Using this method can not only avoid subjective random in the stratigraphic classification in single well, but also can give evidence to field horizon tracing.
实际资料的相干时间剖面表明，该算法有效地突出了地层的高连续性特征，有利于层位追踪和断层解释。
The result of practical coherent time profiles indicates that the new algorithm can effectively enhance the continuity, which is helpful to track strata and explain faults.
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