The Chaobei Region of Anhui Province is tectonically located in the eastern part of the lateMesozoic North China Plateau, to east of the Tanlu fault, and in the northern margin of the Lower Yangtze foldthrust belt of the Yangtze Block in the southern Sulu High Pressure and UltraHigh Pressure orogenic belt. Its evolution is constrained by the tectonic setting and characterized by superimposed faulting structures consisting of two synclines and one anticline. The structure of this kind and concealed structural deformation may attribute to multiphase defomations, including three folding stages in Indosinian and three thrusting related. The firststage deformation is characterized mainly by low angular detachment planes of Lower Siliurian Gaojiabian Formation and the related local faults and faultdetatched folds. The secondstage resulted in the tectonic pattern containing one folding system (two synclines and one anticline) and one NWSEstriking imbricated thrusting complex. The thirdstage is characterized by NWWstriking open folds and lowerangle thrust. During the middle Yanshanian, one NSstriking fold superposed onto the earlier structures. However, the late Yanshanian NWtrending faulting is characterized by NEdipping dominotype normal fault complex in this area, which regionally controls Upper Creatacious depocenter. The regional correlation shows that the Indosinian deformation is in agreement with the SuluDabie deformation, indicating that they are related to exhumation mechanism of the HPUHP rocks in the DabieSulu orogen and that the Yanshanian deformation dynamics is probably related to both the subduction of the PaleoPacific Plate and escaping structure in eastern China.