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1)  crust tilt-lift
地壳掀斜抬升
2)  tilt-lift
掀斜抬升
1.
Crustal tilt-lift and activation are in progress.
现阶段地壳活化,持续掀斜抬升运动。
3)  crustal uplift
地壳抬升
1.
Based on the geometry of the alluvial fan and the erosional features on the top of Maokou Formation, it is suggested that the magnitude of crustal uplift prior to the.
玄武岩喷发前公里规模的地壳抬升是大火成岩省地幔柱成因的一个重要标志,此类地质证据的缺乏反过来被一些学者用来否定地幔柱学说。
2.
The biostratigraphic comparison and sedimentological features of the Maokou limestone in SW China demonstrate that differential erosion and crustal uplift were developed prior to eruption of the Emeishan flood basalts.
差异剥蚀是中二叠世晚期上扬子西缘一次快速地壳抬升和穹状隆起的结果,这说明峨眉山大火成岩省的形成与地幔柱活动有关。
4)  tilting uplift
掀斜隆升
5)  uplift and doming
地壳抬升和穹状隆起
6)  tectonic tilting uplift
构造掀斜隆升
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