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波动是世界上最普遍的运动形式,地壳运动也是以波的形式进行的。新老地层在平面上相间出现,隆起拗陷交替发生,地层的褶皱,断块的上下起伏,都呈现波浪的形式。
Fluctuation is the most common form of movement in the world and crustal movement takes place in the form of waves. The old and new strata appear alternately on the plane and the uplift and depression alternately occur. The folds of the strata and the ups and downs of the fault block all appear in the form of waves.