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.
多波多分量地震地质层位对比是多波地震资料解释和应用中最关键、最基础的工作。
The geologic correlation of multiwave and multicomponent seismic data is the most important and fundamental work.
地震层曲率是根据三维地震解释层位计算得到的曲率，反映解释层位上任一点的弯曲程度。
Seismic horizon curvature is calculated from 3d seismic interpretation horizon and reflects the curving degree to the given horizon at a point.
针对二维地震叠偏剖面解释中存在的断层解释问题，提出了叠偏剖面断层解释方法，阐述了断点解释、组合断层与层位闭合、断面闭合及归位次序之间的关系。
To cope with the fault interpretation problem in interpretation of 2 D stacked migration section, a method is proposed in this paper for fault interpretation.
针对二维地震叠偏剖面解释中存在的断层解释问题，提出了叠偏剖面断层解释方法，阐述了断点解释、组合断层与层位闭合、断面闭合及归位次序之间的关系。
To cope with the fault interpretation problem in interpretation of 2 D stacked migration section, a method is proposed in this paper for fault interpretation.
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