Dayangshu Basin was in extensional setting in the Quaternary period, and a series of small extensional half-grabens were formed.
第四纪大杨树盆地具有伸展的特征，发育一系列小型伸展断陷。
Dayangshu Basin experienced multistage deformations, which is characterized mainly by extensional structures, and was superimposed by compressional structures and positive inversion structures.
大杨树盆地经历了多期变形作用，具有以伸展构造为主、并被挤压构造和反转构造叠加的构造特征。
Dayangshu Basin experienced multistage deformations, which is characterized mainly by extensional structures, and was superimposed by compressional structures and positive inversion structures.
大杨树盆地经历了多期变形作用，具有以伸展构造为主、并被挤压构造和反转构造叠加的构造特征。
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