The diffusion controlled ledge growth mechanism of bainite (DCLGMB) is
reviewed briefly in this paper. It is argued that the existence of the ledge can not prove
the existence of DCLGMB. A growth mode of lower bainite by shearing on the stacking
fault face of austenite is proposed. In this mode, the thickening of lower bainite depends
on the interfacial misfit dislocation loop (IMDL), which expands on the stacking fault
faces of austenite. Ledges move only along the stacking fault faces but not along the side
direction, and the side faces of ledges are not incoherent boundary. The observed
experimental phenomenon of the austenitic stacking fault fringes corresponding to the
lower bainitic growth ledges can be explained by the shear thickening mode.