Rock mass is discontinuous because of the movement and development of the crust. The joint, fissure, fault fracture are the typical modes of this discontinuation.

  • 岩体介质由于地壳的不断运动、发展,呈现出显著的不连续性,存在大量的节理、裂隙等不连续界面。

  • 互联网摘选 2025-01-19 22:40:51

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