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多旋回地形
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多旋回地形
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理学
多旋回地形
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polycyclic landform
多旋回地形
在地形发育过程中,由于地壳运动或自然环境的变化,使内、外营力及其作用强度发生多次变化所形成的地形。又称多循环地形、多轮回地形。
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