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Figure 1
An inverse pole figure map of lath martensite. The martensite grains are identified by a misorientation threshold of 3°. Grain boundaries are in black and zero solutions are in white. The scale bar is 25 µm.

Journal logoJOURNAL OF
APPLIED
CRYSTALLOGRAPHY
ISSN: 1600-5767
Volume 55| Part 1| February 2022| Pages 180-194
https://doi.org/10.1107/S1600576721011560
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