2) tilting tectonic
掀斜构造
3) 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。
4) tilting uplift
掀斜隆升
5) 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。
6) tectonic tilt
构造掀斜
补充资料：掀掀
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