地壳运动引起的地壳变形变位,是地壳运动的“足迹”,也是地壳运动的证据。在地质构造剖面图上,只要有断裂面,且同一岩层沿断裂面两侧发生错动,即为断层(无论两侧岩层向上还是向下弯曲)。无论岩层如何缺失,只要用虚线将同一岩层恢复连接起来后,是波状曲线,即为褶皱。其中岩层向 Crustal deformation caused by crustal movement is the “footprints” of crustal movement and evidence of crustal movement. In the geological structure of the profile, as long as there is a fracture surface, and the same rock along the fracture surface on both sides of the dislocation, is the fault (regardless of both sides of the rock up or down bending). No matter how the rock formation is missing, as long as the same rock formation is connected with a dashed line, it is a wavy curve, which is the fold. Among the rock formations