Confocal μ-XANES as a tool to analyze Fe oxidation state in heterogeneous samples: the case of melt inclusions in olivine from the Hekla volcano

Here we present a confocal Fe K-edge μ-XANES method (where XANES stands for X-ray absorption near-edge spectroscopy) for the analysis of Fe oxidation state in heterogeneous and one-side-polished samples. The new technique allows for an analysis of small volumes with high spatial 3D resolution of <...

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Bibliographic Details
Main Authors: Botcharnikov, Roman, Wilke, Max, Garrevoet, Jan, Portnyagin, Maxim, Klimm, Kevin, Buhre, Stephan, Krasheninnikov, Stepan, Almeev, Renat, Moune, Severine, Falkenberg, Gerald
Format: Article in Journal/Newspaper
Language:English
Published: Johannes Gutenberg-Universität Mainz 2024
Subjects:
ddc:550
Hekla
Iceland
Online Access:https://openscience.ub.uni-mainz.de/handle/20.500.12030/11323
https://hdl.handle.net/20.500.12030/11323
https://doi.org/10.25358/openscience-11302
Description
Summary:Here we present a confocal Fe K-edge μ-XANES method (where XANES stands for X-ray absorption near-edge spectroscopy) for the analysis of Fe oxidation state in heterogeneous and one-side-polished samples. The new technique allows for an analysis of small volumes with high spatial 3D resolution of <100 µm3. The probed volume is restricted to that just beneath the surface of the exposed object. This protocol avoids contamination of the signal by the host material and minimizes self-absorption effects. This technique has been tested on a set of experimental glasses with a wide range of Fe3+ ΣFe ratios. The method was applied to the analysis of natural melt inclusions trapped in forsteritic to fayalitic olivine crystals of the Hekla volcano, Iceland. Our measurements reveal changes in Fe3+ ΣFe from 0.17 in basaltic up to 0.45 in dacitic melts, whereas the magnetite–ilmenite equilibrium shows redox conditions with Fe3+ ΣFe ≤0.20 (close to FMQ, fayalite–magnetite–quartz redox equilibrium) along the entire range o

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