1) tilting deformation
掀斜变形
1.
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。
2) Deformation mechanism and failure
掀斜-沉陷变形
3) Tip-tilting Movement
掀斜变动
5) tilting tectonic
掀斜构造
6) tilted fault block
掀斜断块
1.
Based on volcanic activities and tectonic evolution,it is suggested that the tilted fault block,sliding structures in extensional setting should be developed in Cretaceous to Cenozoic age.
结合区域火山活动和构造演化认为,该滑动构造为伸展背景下的掀斜断块型,其滑动时间为白垩纪—新生代。
补充资料：掀掀
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