The location of Mn and Fe in axinite–(Fe) from Nandan, China determined by anomalous X–ray scattering (AXS)
Author:
Affiliation:
1. Institute for Materials Research (IMR), Tohoku University
2. Neutron Science and Technology Center, CROSS
3. The University Museum, The University of Tokyo
Publisher
Japan Association of Mineralogical Sciences
Subject
Geology,Geophysics
Link
https://www.jstage.jst.go.jp/article/jmps/115/3/115_190110/_pdf
Reference21 articles.
1. Andreozzi, G.B., Ottolini, L., Lucchesi, S., Graziani, G. and Russo, U. (2000a) Crystal chemistry of the axinite–group minerals: A multi–analytical approach. American Mineralogist, 85, 698–706.
2. Andreozzi, G.B., Lucchesi, S. and Graziani, G. (2000b) Structural study of magnesioaxinite and its crystal–chemical relations with axinite–group minerals. European Journal of Mineralogy, 12, 1185–1194.
3. Andreozzi, G.B., Lucchesi, S., Graziani, G. and Russo, U. (2004) Site distribution of Fe2+ and Fe3+ in the axinite mineral group: New crystal–chemical formula. American Mineralogist, 89, 1763–1771.
4. Basso, R., Della Giusta, A. and Vlaic, G. (1973) La struttura della tinzenite. Periodico di Mineralogia, 42, 369–379.
5. Belokoneva, E.L., Pletnev, P.A. and Spiridonov, E.M. (1997) Crystal structure of low–manganese tinzenite (severginite). Crystallography Reports, 42, 934–937.
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1. In-house-built single-crystal anomalous X-ray diffraction measurement system using white X-rays and an energy dispersive detector;Journal of the Ceramic Society of Japan;2021-09-01
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