1) Tip-tilting Movement
掀斜变动
2) 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。
3) tilting movement
掀斜运动
1.
through the observation and research in Songshan area in last several years, the authors discussed the characteristics of neotectonic movement, which are mainly intermittent uplifts and tilting movement.
根据几年来对嵩山地区的考察和研究 ,通过对夷平面、河流阶地、串珠状洪积扇等诸多地貌现象的分析 ,论述了嵩山地区新构造运动以间歇性抬升运动和掀斜运动为主的特征。
4) Deformation mechanism and failure
掀斜-沉陷变形
6) tilt movement
旋张掀斜运动
1.
The tilt movement of the Ryukyu island-arc system toward the ocean trench and the waving movement of the mantle stream in the island-arc-back-arc area are the power source of the movement of the Okinawa Trough.
琉球岛弧系向海沟方向的旋张掀斜运动和岛弧-弧后地区地幔流的波动运动是冲绳海槽张裂运动的动力源。
补充资料：掀掀
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参考词条