Abstract
In order to investigate the role of {101} α type twins or faults observed at the periphery of the martensite plate, the structure of the martensite in a 1.80 mass% C steel with a high tetragonality of 1.078 was studied by transmission electron microscopy, and in terms of the phenomenological theory of martensitic transformation. The periphery of the martensite contained two or three kinds of {101} α twins or faults in additon to the transformation twins of the (112)[111], system concentrated in the midrib
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