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X-ray diffraction and zero-field NMR spectra were studied for powdered and bulk polycrystalline and single-crystal specimens of cobalt. The nature of the h.c.p.-f.c.c. phase transition was studied. It is shown that the two stacking fault NMR lines are both due to deformation faults in h.c.p. regions.
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Creagh et al. (1975) studied this question.
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