Fe K-EDGE X-RAY ABSORPTION SPECTROSCOPY OF SILICATE MINERALS AND GLASSES

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Binsted , N.; Greaves , G.; Henderson , C.;
(1986)

Structural parameters determined for crystalline iron, fayalite and aegirine agree closely with X-ray crystallograhic data. A glass of NaFeSi2O6 composition has Fe predominantly present as Fe3+ in tetrahedral coordination i.e. as a network former. CaFeSiO4 and CaFeSi2O6... View more
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    and Henderson, C.M.B. Progr. Expt. Petrology Apted, M.J., and Brown, G.E. Phys. Chem. Minerals, 10, 1

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