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• W2010732051 abstract "We present a x-ray magnetic circular dichroism (XMCD) study performed at the Fe K edge in R6Fe23 compounds exhibiting magnetic compensation (R=Ho and Y). The Fe K-edge XMCD signal has been identified as due to both Fe itself and rare-earth contributions. Following a simple two-sublattices model for the analysis of the dichroic signal the contribution of the rare-earth sublattice to total Fe K-edge XMCD signal has been extracted and proven to be directly correlated to the R magnetic moment." @default.
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• W2010732051 date "2000-07-01" @default.
• W2010732051 modified "2023-10-03" @default.
• W2010732051 title "Fe <i>K</i>-edge x-ray magnetic circular dichroism study in R6Fe23 (R=Ho and Y) compounds near compensation temperature" @default.
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• W2010732051 doi "https://doi.org/10.1063/1.373663" @default.
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