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
石力学问题的最大障碍是体的非
质及其包含的大量节理断层，本文采多
域思想结合节理断层的非线性模型较好地解决了这一难题。
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.
边界元法广泛应石力学问题的最大障碍是体的非质及其包含的大量节理断层，本文采多域思想结合节理断层的非线性模型较好地解决了这一难题。
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