Structural environment of iron and accurate determination of Fe3+/ΣFe ratios in andesitic glasses by XANES and Mössbauer spectroscopy-Reference-Cited by-同舟云学术

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Structural environment of iron and accurate determination of Fe3+/ΣFe ratios in andesitic glasses by XANES and Mössbauer spectroscopy

Published:2016-06 Issue: Volume:428 Page:48-58
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Zhang H.L.,Hirschmann M.M.,Cottrell E.,Newville M.,Lanzirotti A.

Funder

NASA

NSF

GUP

Department of Energy (DOE) — Geosciences

DOE

National Science Foundation — Earth Sciences

Department of Energy — GeoSciences

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference70 articles.

1. Analysis of Mössbauer spectra of silicate glasses using a two-dimensional Gaussian distribution of hyperfine parameters;Alberto;J. Non-Cryst. Solids,1996

2. Repeated recharge, assimilation, and hybridization in magmas erupted from El Chichón as recorded by plagioclase and amphibole phenocrysts;Andrews;J. Volcanol. Geotherm. Res.,2008

3. Oxidation status of the mantle: past and present;Arculus;Annu. Rev. Earth Planet. Sci.,1985

4. XANES calibrations for the oxidation state of iron in a silicate glass;Berry;Am. Mineral.,2003

5. The Fe3+/ΣFe ratios of MORB glasses and their implications for mantle melting;Bézos;Geochim. Cosmochim. Acta,2005

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