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
的最大障碍是岩体的
及其包含的大量节理断层，本文采用多子域思
结合节理断层的线性模型较好地解决了这
。
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的最大障碍是岩体的及其包含的大量节理断层，本文采用多子域思结合节理断层的线性模型较好地解决了这。
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