High‐Pressure XAFS Measurements of the Coordination Environments of Fe <sup>2+</sup> and Fe <sup>3+</sup> in Basaltic Glasses-Reference-Cited by-同舟云学术

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High‐Pressure XAFS Measurements of the Coordination Environments of Fe ²⁺ and Fe ³⁺ in Basaltic Glasses

Published:2022-04 Issue:4 Volume:127 Page:
ISSN:2169-9313
Container-title:Journal of Geophysical Research: Solid Earth
language:en
Short-container-title:JGR Solid Earth

Author:

Ozawa Keisuke¹^ORCID,Hirose Kei¹²^ORCID,Takahashi Yoshio¹³^ORCID

Affiliation:

1. Department of Earth and Planetary Science The University of Tokyo Tokyo Japan

2. Earth‐Life Science Institute Tokyo Institute of Technology Tokyo Japan

3. Institute of Materials Structure Science High‐Energy Accelerator Research Organization Tsukuba Japan

Publisher

American Geophysical Union (AGU)

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2021JB023902

Reference54 articles.

1. High-pressure Raman spectroscopy of diamond anvils to 250GPa: Method for pressure determination in the multimegabar pressure range

2. Local structural variation with oxygen fugacity in Fe2SiO4+ fayalitic iron silicate melts

3. Iron K-edge X-ray absorption near-edge structure spectroscopy of aerodynamically levitated silicate melts and glasses

4. Deep magma ocean formation set the oxidation state of Earth’s mantle

5. Iron Partitioning in Earth's Mantle: Toward a Deep Lower Mantle Discontinuity

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1. Pressure dependence of metal–silicate partitioning explains the mantle phosphorus abundance;Scientific Reports;2024-01-12

2. Determination of Fe2+ in tin oxide-containing glass through valence-selective solvent extraction and colorimetric analysis following glass decomposition;Chemistry Letters;2023-12-01

3. Spectroscopic Characterization of Impactites and a Machine Learning Approach to Determine the Oxidation State of Iron in Glass‐Bearing Materials;Journal of Geophysical Research: Planets;2023-03

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