Deformation twinning in a medium carbon steel containing ferrite and pearlite under shock compression is investigated below and above the α–ε phase transition stress (σT), within a peak stress range of 10–20 GPa. Free surface velocity histories are measured to obtain the Hugoniot elastic limit (2.7 GPa), σT (13.3 GPa) and bulk plastic strain. Postmortem samples are characterized with electron backscatter diffraction and transmission electron microscopy. Below σT, all the {112}〈111〉 twinning activation in ferrite and pearlite follows the Schmid law, while above σT, approximately 1/6 of the activation deviates from the law. Propagation of the {112}〈111〉 twins in pearlite depends on the orientation of the activated twinning plane relative to cementite lamellae. With increasing peak stress, the {112}〈111〉 twin area fraction in ferrite/pearlite increases greatly/slightly; the {112}〈111〉 twin area fraction in ferrite is about 7 times that of pearlite. The {332}〈113〉 twins can only form above σT, favoring ferrite over pearlite, and are likely to be the secondary twins originated at the {112}〈111〉 twin boundaries.
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