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Anisotropic microstrain broadening in cementite, Fe3C, caused by thermal microstress: comparison between prediction and results from diffraction-line profile analysis

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Leineweber,  A.
Dept. Phase Transformations; Thermodynamics and Kinetics, Max Planck Institute for Intelligent Systems, Max Planck Society;

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Leineweber, A. (2012). Anisotropic microstrain broadening in cementite, Fe3C, caused by thermal microstress: comparison between prediction and results from diffraction-line profile analysis. Journal of Applied Crystallography, 45, 944-949. doi:10.1107/S0021889812036862.


Cite as: https://hdl.handle.net/11858/00-001M-0000-000E-BACC-B
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