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力综合作用的前陆地。
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的基础上,得出地是一个受多方向挤压力综合作用的前陆地。
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