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Cation preferences in thio-olivines (Fe1-xMnx)(2)SiS4, x <= 0.50, studied by Mossbauer spectroscopy at room temperature
Uppsala University, Teknisk-naturvetenskapliga vetenskapsområdet, Earth Sciences, Department of Earth Sciences.
2001 (English)In: NEUES JAHRBUCH FUR MINERALOGIE-MONATSHEFTE, ISSN 0028-3649, no 9, 403-413 p.Article in journal (Refereed) Published
Abstract [en]

Synthetic (Fe1-xMnx)(2)SiS4, Mn = 0, 0.01, 0.02, 0.05, 0.10, 0.20, 0.50, with olivine structure, Pnma, has been synthesized using quartz-ampoule techniques. The powder materials have been characterized, using X-ray diffraction (XRD) and Mossbauer spectros

Place, publisher, year, edition, pages
E SCHWEIZERBARTSCHE VERLAGS , 2001. no 9, 403-413 p.
Keyword [en]
thio-olivine; olivine structure; cation distribution; Mossbauer spectroscopy; X-ray diffraction; FE2SIS4
URN: urn:nbn:se:uu:diva-37826OAI: oai:DiVA.org:uu-37826DiVA: diva2:65725
Addresses: Ericsson T, Uppsala Univ, Dept Earth Sci, Villavagen 16, SE-75236 Uppsala, Sweden. Uppsala Univ, Dept Earth Sci, SE-75236 Uppsala, Sweden.Available from: 2008-10-17 Created: 2008-10-17 Last updated: 2011-01-14

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