“…New X-ray observations now give direct evidence that the loss of tetragonality of martensite during the first tempering stage is due to the precipitation of a close-packed hexagonal iron carbide which it is proposed should be named e-iron carbide, or e-Fe3C, because of its structural similarity with e-Fe3N, e-Iron carbide is formed as a coherent transitional phase in which the Laue condition for X-ray reflexion is obeyed preferentially in a direction normal to the (101) (Jack, 1948 b) at their lower interstitial-atom concentration limit, Fea(C,N ). A similar iron carbide, Fe2C, has been described by Hofer, Cohn & Peebles (1949) as the carbonrich extreme of the same carbonitride series at its upper interstitial-atom concentration limit, F%(C, N).…”