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应用马尔柯夫过程理论和计算机技术分析了地层岩性序列．提出一种根据转移概率矩阵和熵分析确定给定层段地层沉积旋回性质的新方法，通过对两口井九个井段资料的实际处理，证明该方法是可行的，计算机解释结果与手工解释结果完全吻合。
Stratigraphic lithology sequence is analyzed by using Markov process theory and computer technology. A new method to determine the cyclostation of sedimentary strata in a given interval based on transfer probability matrix and entropy analysis is proposed. The actual treatment of data from nine intervals in two wells shows that the method is feasible. The results of computer interpretation and manual interpretation Exactly match.