Site soils in southern area of Jiangsu province belong to washland sediment or limnetic facies sediment.The components of sediment are very complex and process of sedimentation is in disorder.
英
美
- 蘇南地區場(chǎng)地土主要為漫灘相、湖沼相或沖湖相新近沉積軟弱土,結構松散,沉積零亂,成分復雜,飽水可液化粉細砂層及粉土層較為發(fā)育,在地震或動(dòng)力荷載的作用下有可能發(fā)生軟土震陷或砂土液化。
