MAGNETIC HYPERFINE FIELD DISTRIBUTION IN PYRRHOTITES FROM MOSSBAUER-SPECTROSCOPYстатья
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Аннотация:Mossbauer spectra from intermediate pyrrhotite (Fe(1-x)S) samples were interpreted according to their hyperfine magnetic field distribution functions at the Fe nuclei in these sulfides. Seven non-equivalent Mossbauer sites for Fe were distinguished by their peak positions in the distribution functions obtained.