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第四纪夷平面
释义
第四纪夷平面
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理学
地貌学
释
planation surface
第四纪夷平面
在地壳运动相对稳定的构造地质背景条件下,受海平面或局地侵蚀基准所控制,经过长时间的风化、剥蚀和侵蚀等外动力地质作用改造,横切不同地质时期的地层与构造后形成的大范围、低起伏的平缓陆地地形。又称均夷面。
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