运用这一关系可通过层速度预测断裂的封闭性。
Hence the sealing capacity of faults can be predicted by seismic interval velocity.
通过层序地层学研究，产生于可对比不整合广泛分离的沉积物可以彼此比较。
Through sequence stratigraphy, widely-separated sediments that occur between correlatable unconformities could be compared with each other.
本文在均匀化方法的基础上，通过层合结构的均匀化基元，建立相应的有限元方法，对层合板进行损伤刚度分析。
By this method, combining with the finite element method, the homogenized mixing unit cell is solved to perform damaged stiffness analysis.
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