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The effect of uniaxial stress on the high-field magnetoresistance anisotropy of iron is measured and shown, by a combination of group theory and a band-structure interpolation scheme, to correspond to the origin of the (100) open orbits being magnetic breakdown between the hole octahedron and the electron jack on the minority-spin Fermi surface.
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Angadi et al. (1974) studied this question.
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