Displacive transformations have been widely reported in metals, alloys and ceramics, but rarely reported to be important in the aqueous corrosion of alloys. We report here our analysis of the formation of the hexagonal-ZrO suboxide during the aqueous corrosion of α-Zr alloys and propose this to be a paraequilibrium displacive transformation with the rate controlled by oxygen diffusion. Two orientation relationships were identified between α-Zr and hexagonal-ZrO,(0002) α− Z r∥(1¯ 011) h− Z r O and [2¯ 110] α− Z r∥[10 1¯ 2] h− Z r O or (0002) α− Z r∥(22 4¯ 1¯) h− Z r O and [2¯ 110] α− Z r∥[1 1¯ 01] h− Z r O, with the first one more commonly observed. No specific orientation relationships between either hexagonal-ZrO and monoclinic-ZrO 2 or α-Zr and monoclinic-ZrO 2 were identified, which suggests that the formation of often-reported bulk oxide texture during aqueous corrosion is not related directly to the texture of the metallic substrate. These results provide a guideline for understanding the mechanisms of crystallographic evolution during oxide growth on commercial zirconium alloys, and also demonstrate the capability of transmission Kikuchi diffraction to investigate orientation relationships in nano-scale materials.