This paper presents an efficient method of modelling jointed rock by using the boundary ele-ment method via the concept of multiregion and non-linear model of joint and fault.
边界元法广泛应用于岩石力学问题最大障碍是岩体
非均质及其包含
大量节理断层,本文采用
域思想结合节理断层
非线性模型较好地解决了这一难题。