造山运动
造山运动（Orogeny）是指地壳结构因为板块运动产生剧烈变化，属地壳变动个一种。迭种作用会产生岩石高度变形个带状区域，称为造山带（Orogens或Orogenic belts）。“Orogeny”来自希腊语，“oro”是山，“geny”是“genesis”个略语，诞生或起源个意思。
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