地震层位标定是连接地质、测井和地震资料的有效方法。
Seismic layer labeling is an effective method for connecting geologic, logging and seismic data.
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.
本文针对特定的地震层位使用连续介质线弹性有限元模型，计算了研究区内主应力和剪切应力的分布。
The distributions of dominant stress and shear stress in research area of a given seismic horizon are estimated by using linear elastic finite element modeling in continuous medium.
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