摘要
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。
The lithological seqence is analyzed on computer according to Markov processtheorv. A new method of autodetermining sedimentary cycles of the given intervals is studiedby the use of transition probability and entropy funcuon The data of nine intervals in twowells are processed by computer.The results of computer processing are in good agreementwith that of human works.
出处
《石油大学学报（自然科学版）》
CSCD
1994年第6期36-39,共4页
Journal of the University of Petroleum,China(Edition of Natural Science)
