Multiple methods were applied to study the deformation characteristics of hornblende in Archean plagioamphibolite mylonite from the Western Hills(Beijing),including optical microscopy(OM),electron backscatter diffraction(EBSD),transmission electron microscopy(TEM),and electron probe microanalysis(EPMA).The hornblendes are σ and δ type porphyroclasts with the new-born needle shaped grains as their tails.The analysis of lattice preferred orientation(LPO) of both the porphyroclasts and the new-born grains shows that the main slip system of the deformed hornblende is(100)<001>,suggesting that the fabric characteristics of new-born grains inherit that of porphyroclasts.Sub-microstructures show the porphyroclast core is dominated by dislocation tangle,little or no dislocations in the new-born grains,and the subgrains confined by dislocations in the transition zone between porphyroclasts and new-born grains.By using plagioclase-hornblende geothermometry and hornblende geobarometry,the estimated temperature and pressure of porphyroclasts are 675.3-702.9℃ and 0.29-0.41 GPa and those of new-born grains are 614.1-679.0℃ and 0.11-0.31 GPa.The bulging recrystallization is summarized as deformation mechanisms of hornblende by the discussions of the microstructures,EBSD fabric,sub-microstructures,and the deformed temperature and pressure. Multiple methods were applied to study the deformation characteristics of hornblende in Archean plagioamphibolite mylonite from the Western Hills (Beijing), including optical microscopy (OM), electron backscatter diffraction (EBSD), transmission electron microscopy (TEM), and electron probe microanalysis ). The hornblendes are σ and δ type porphyroclasts with the new-born needle shaped grains as their tails. The analysis of lattice preferred orientation (LPO) of both the porphyroclasts and the new-born grains shows that the main slip system of the deformed hornblende is (100) <001>, suggesting that the fabric characteristics of new-born grains inherit that of porphyroclasts. Sub-microstructures show the porphyroclast core is dominated by dislocation tangle, little or no dislocations in the new-born grains, and the subgrains confined by dislocations in the transition zone between porphyroclasts and new-born grains. By using plagioclase-hornblende geothermometry and hornblende geobarometry, the estim ated temperature and pressure of porphyroclasts are 675.3-702.9 ° C and 0.29-0.41 GPa and those of new-born grains are 614.1-679.0 ° C and 0.11-0.31 GPa. The bulging recrystallization is summarized as deformation mechanisms of hornblende by the discussions of the microstructures , EBSD fabric, sub-microstructures, and the deformed temperature and pressure.