The Qiongdongnan Basin is a Tertiary extensional basin developed on the north margin of South China Sea, with a main structural style of half-grabens. Three types of half-grabens have been identified after analyzing the geometry of the half-grabens from the seismic sections in the basin. The half-grabens mainly experienced two evolutionary stages. The tectonic history of the basin shows two stages of extension based on the integrated research of half-grabens and regional tectonic dynamics. In addition, symmetrical distribution of the half-grabens and crust structure indicated the stretching style of the basin is pure shear.