Abstract
Spectroscopic study of two diselenide compositions (Cu,Fe)Se2-x, differing slightly in M/Se ratio, showed Fe in only one site of the pyrite-like structure. Isomer shift values support the occurrence of low-spin Fe2+ in the octahedral sites. All the compositions centred around CuFeSe2 show complex spectra believed to represent the onset of a magnetic ordering transition just below room T.-R.A.H.
Original language | English |
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Pages (from-to) | 1407-1412 |
Number of pages | 6 |
Journal | Rendiconti della Societa Italiana di Mineralogia e Petrologia |
Volume | 38 |
Issue number | 3 |
Publication status | Published - 1983 |