Mössbauer Study of Oxidized Iron Silicate Minerals
- 1 January 1969
- journal article
- research article
- Published by Wiley in Physica Status Solidi (b)
- Vol. 33 (2) , 741-748
- https://doi.org/10.1002/pssb.19690330227
Abstract
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.Keywords
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