建立统一标准的地震记录极性和层位标定是精细地震解释的两项基础工作。
Standard polarity establishment and horizon identification are two essentials in meticulous seismic data interpretation.
地震层位标定是地震资料构造解释和地震储层研究的基础。
Seismic horizons labeling is basis of structural interpretation of seismic data and study of seismic reservoir.
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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