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Cation preferences in thio-olivines (Fe1-xMgx)(2)SiS4, x <= 0.30, studied by Mossbauer spectroscopy at room temperature
Uppsala University.
Uppsala University.
Uppsala University.
1999 (English)In: NEUES JAHRBUCH FUR MINERALOGIE-MONATSHEFTE, ISSN 0028-3649, no 11, p. 518-528Article in journal (Other scientific) Published
Abstract [en]

Synthetic (Fe1-xMgx)(2)SiS4, Mg = 0.10, 0.20, 0.30, with olivine structure, Pnma, has been synthesized using quartz-ampoule technique. The powder materials have been characterized, using X-ray diffraction (XRD) and Mossbauer spectroscopy techniques. The c

Place, publisher, year, edition, pages
E SCHWEIZERBARTSCHE VERLAGS , 1999. no 11, p. 518-528
Keywords [en]
thio-olivine; olivine structure; cation distribution; Mossbauer spectroscopy; X-ray diffraction; IONIC-RADII; SILICATE; MN
Identifiers
URN: urn:nbn:se:uu:diva-27698OAI: oai:DiVA.org:uu-27698DiVA, id: diva2:55594
Note
Addresses: Ericsson T, Uppsala Univ, Dept Earth Sci Mineral Petrol, Villavagen 16, SE-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci Mineral Petrol, SE-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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