1.From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.
在与国外前陆盆的基础上,得出四川盆是一个受多方向挤压应力综合作用的前陆盆。
2.The area had undergone such evolution stages as passive borderland basining, squeerze-retrograde nose-like swelling, cratonic inner sagging. intracratonic basining and para-foreland basin.