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的基础上，得出四川盆地是一个受多方向挤压应力综合作用的前陆盆地。

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.

在与国外前陆地对比的基础上，得出地是一个受多方向挤压应力综合作用的前陆地。

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.

克拉内凹陷段；克拉内坳陷地段和类前陆地段。

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

在与国外前陆盆地对比的基础，四川盆地是一个受多方向挤压应力综合作用的前陆盆地。

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；克拉内坳陷盆地发展阶和类前陆盆地发展阶。

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

在与国外前陆地对比的基础上，得出四川地是一个受多方向挤压应作用的前陆地。

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.

克拉内凹阶段；克拉内地发展阶段和类前陆地发展阶段。

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.

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

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.

在前陆盆地对比的基础上，得出四川盆地是一个受多方向挤压应力综合作用的前陆盆地。

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.

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

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.

在与国外前陆盆地对比的基础上，得出四川盆地是一个受挤压应力综合作用的前陆盆地。

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；克拉内坳陷盆地发展类前陆盆地发展。

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的基础，四川盆地是一个受多方向挤压应力综合作用的前陆盆地。

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；克拉内坳陷盆地发展阶和类前陆盆地发展阶。