Distribution of Fe3+ in a synthetic (Ca,Na)2(Mg,Fe3+)Si2O7-melilite: 57Fe Mössbauer and X-ray Rietveld studies
Author:
Affiliation:
1. Department of Materials Creation Technology, Graduate School of Science and Engineering, Shimane University
2. Department of Geology, Faculty of Science, Shinshu University
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/100/6/100_6_229/_pdf
Reference38 articles.
1. Akasaka, M. and Ohashi, H. (1985) 57Fe Mössbauer study of synthetic Fe3+-melilites. Physics and Chemistry of Minerals, 12, 13-18.
2. Akasaka, M., Ohashi, H. and Shinno, I. (1986) The distribution of Fe3+ and Ga3+ between two tetrahedral sites in melilites, Ca2(Mg,Fe3+,Ga,Si)3O7. Physics and Chemistry of Minerals, 13, 152-155.
3. Akasaka, M. and Shinno, I. (1992) Mössbauer spectroscopy and its recent application to silicate mineralogy. Journal of Mineralogical Society of Japan, 21, 3-20 (In Japanese with English abstract).
4. Armbruster, T., Röthlisberger, F. and Seifert, F. (1990) Layer topology, stacking variation, and site distortion in melilite-related compounds in the system CaO-ZnO-GeO2-SiO2. American Mineralogist, 75, 847-858.
5. Bancroft, G.M., Maddock, A.G. and Burns, R.G. (1967) Applications of the Mössbauer effect to silicate mineralogy - I. Iron silicates of known crystal structure. Geochimica et Cosmochimica Acta, 31, 2219-2246.
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