地;
纹;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
基础上，得出
地是一个受多方向挤压应力综合作用前陆地。
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基础上，得出地是一个受多方向挤压应力综合作用前陆地。
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