There is a large numbers of mantle xenoliths derived from the Cenozoic basalt in Huinan, Jilin province. The mantle xenoliths are dominated by spinel lherzolite. Equilibrium temperature calculated by the mineral chemical compositions show that temperature is within the range of 982-1085 ℃. As revealed by the oxidation decoration technique, the samples have undergone dislocation creep dominated plastic deformation, resulting in different kinds of the dislocation structures. By using the size of subgrain, the differential stress of olivine is estimated to be in the range of 21.3-36.5 MPa. The LPOs of olivine, which is measured by the EBSD technique，show A-type olivine fabrics as a whole. The variation of temperature and fabric and seismic anisotropy of LQLW08-18 suggest that the temperature may have a effect in preference to the [100] crystal axis. According to the study of olivine and peridotite anisotropy and the mineral compositions in the peridotite, the orthopyroxene can reduce the overall effect of the anisotropy. Different kinds of rheological parameters and fabrics characteristics not only provide basic information and restrictions for the further study of the upper mantle but also show the mantle heterogeneity and the replacement (chemical erosion) may be the main dynamic mechanism of destruction in this area.