云南夷平面
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The planation surface in west Yunnan was universally deformed, and the deformation is generally belonging to two types; one is the large area tilting deformation.
夷平面普遍受到两种变形，一种是大面积的掀斜变形，夷平面高度由西北向东南方向递减；另一种为断裂变形，夷平面呈地堑式下降或地垒式上升。
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