盆地内地质构造断裂和采煤活动中产生的采动断裂互相叠加，构成了十分复杂的地下断裂网络。
The move crevasse superimposes mutually and constitutes the complex underground crevasse network, which are produced by geologic structure crevasse in Fuxin Basin and mining coal.
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.
川西北盆地在新生代是一个典型的构造叠加区域，来自龙门山和米仓山的变形在此相互作用。
The Northwest Sichuan Basin is a typical tectonic superposition region in Cenozoic, where the deformations transferred from the Longmenshan and Micangshan affected together.
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