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。

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.

克拉内凹陷阶段；克拉内坳陷盆发展阶段和类前陆盆发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外前对比的基础上，得出四川个受多方向挤压应力综合作用的前。

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.

克拉内凹陷阶段；克拉内坳陷发展阶段和类前发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外前陆对比的基础上，得出四川是一个受多方向挤综合作用的前陆。

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.

克拉内凹陷阶段；克拉内坳陷展阶段和类前陆展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外陆盆地对比基础上，得出四川盆地是一个受多方向挤压应力综合作陆盆地。

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.

内凹陷阶段；内坳陷盆地发展阶段和类陆盆地发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外地对比的基础上，得出四川地受多方向挤压应力综合作用的地。

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.

克拉内凹陷阶段；克拉内坳陷地发展阶段和类地发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外前陆盆对比的基础上，得出四川盆是一个受多方向挤压应力综合作用的前陆盆。

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.

阶段；坳盆发展阶段和类前陆盆发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外盆地对比基础上，得出四川盆地是一个受多方向挤压应力综合作用盆地。

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.

内凹陷阶；内坳陷盆地发展阶和类盆地发展阶。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外前陆盆地对比，得出四川盆地是一个受多方向挤压应力综合作用前陆盆地。

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.

克拉内凹陷阶段；克拉内坳陷盆地发展阶段和类前陆盆地发展阶段。

From the correlation with foreland basins abroad it is concluded that Sichuan basin resulted from Polydirectional compression stress.

在与国外前陆对比的基础上，得出四川是一个受多方向挤综合作用的前陆。

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.

克拉内凹陷阶段；克拉内坳陷展阶段和类前陆展阶段。