摘要
大试件单轴蠕变实验表明,板岩流动变形破坏受结构面控制。即使在同一方向应力作用下,也表现了平行走向、反倾向、顺倾向方向的差异。这是板岩流动变形破坏各向异性的另一种表现形式。
Large samples uniaxial compressive creep test indicates, the flow deformation and failure of slate is controlled by its structure plane. Although under the same directions stress,it also whows the differences among the parallel strike direction,reverse strike direction and trend direction. This is another appearence of slate flow deformation and failures anisotropy.
出处
《水文地质工程地质》
CAS
CSCD
1997年第5期46-48,共3页
Hydrogeology & Engineering Geology
基金
国家自然科学基金