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Mössbauer Study of Oxidized Iron Silicate Minerals
Author(s) -
Häggström L.,
Wäppling R.,
Annersten H.
Publication year - 1969
Publication title -
physica status solidi (b)
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.51
H-Index - 109
eISSN - 1521-3951
pISSN - 0370-1972
DOI - 10.1002/pssb.19690330227
Subject(s) - amphibole , ferrous , ferric iron , mössbauer spectroscopy , silicate , ferric , chemistry , mineralogy , inorganic chemistry , materials science , metallurgy , crystallography , quartz , organic chemistry
Biotites and Ca‐amphiboles have been studied. Certain changes in composition of the Ca‐amphiboles could be correlated to changes in the Mössbauer parameters. The ordering of iron in biotites is discussed. The ferrous‐ferric iron ratio could be determined in all the silicates.