In this paper, Seismological Network (2007-12-01-2013-12-31) data from Hubei and its surrounding areas are analyzed via the seismic anisotropy method. Shear-wave splitting parameters from 16 stations are obtained. The results show some S-wave splitting phenomena in Hubei and its surrounding areas, and that the dominant directions of fast shear-wave polarization are the northeast and or nearly northsouth directions and there is no first advantage of polarization direction obviously. The stress field of the stations may be the comprehensive result of regional tectonic background stress environments and induced local fractures. Complex local structures may affect the shear-wave splitting results by reducing the dominant polarization direction, which is not in accordance with the strike of the main active faults. Significant differences between the regional principal compressive stress and dominant polarization direction may also affect the results.