The stratum of Early Carboniferous structural level occurred strongly compressive deformation, there are closed anticline and syncline and complexity inter-layer fold, in addition, the sharp edges-like fold exist locally. Late Carboniferous structural layer includes the Upper Carboniferous Xibeikulasi Formation and Tailegula Formation. Obviously the two formations belong to different tectonic deformation levels, which represent the extension of a major movement at the end of Early Carboniferous. It has great significance for clarifying the sequence relationship between Xibeikulasi Formation and Tailegula Formation.