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造陸運動
释义
造陸運動
zào lù yùn dòng
由于地球内部的变化,地壳不断作极为缓慢的升降运动,使海水退出或侵入陆地。广域性的地壳缓慢垂直升降运动,可发生广泛的挠曲或倾斜,造成广大的波状起伏地形。
造陆运动
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更新时间:2025/6/14 2:53:28