Articles | Volume 35, issue 4
https://doi.org/10.5194/ejm-35-549-2023
© Author(s) 2023. This work is distributed under the Creative Commons Attribution 4.0 License.
Research article
| 
31 Jul 2023
Research article |
| 31 Jul 2023
| 31 Jul 2023
Effect of oxygen fugacity on the storage of water in wadsleyite and olivine in H and H–C fluids and implications for melting atop the transition zone
Related subject area
Mantle petrology and geochemistry
Iron oxidation state in serpentines and magnesian chlorites of subduction-related rocks
Relatively oxidized conditions for diamond formation at Udachnaya (Siberia)
Ab initio thermal expansion and thermoelastic properties of ringwoodite (γ-Mg2SiO4) at mantle transition zone conditions
Eur. J. Mineral., 34, 645–656, 2022
Eur. J. Mineral., 34, 549–561, 2022
Eur. J. Mineral., 34, 167–182, 2022
Cited articles
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A model for the internal cycle of water, Phys. Earth Planet. Int., 322, 106815, https://doi.org/10.1016/j.pepi.2021.106815,
2022.
Balan, E., Blanchard, M., Lazzeri, M., and Ingrin, J.: Theoretical Raman
spectrum and anharmonicity of tetrahedral OH defects in hydrous forsterite,
Eur. J. Miner., 29, 201–212, 2017.
Bali, E., Bolfan-Casanova, N., and Koga, K. T.: Pressure and temperature
dependence of H solubility in forsterite: An implication to water activity
in the Earth interior, Earth Planet. Sc. Lett., 268, 354–363, 2008.
Bercovi, D. and Karato, S.: Whole mantle convection and the transition-zone
water filter, Nature, 425, 39–44, 2003.
Bolfan-Casanova, N., Montagnac, G., and Reynard, B.: Measurement of water
contents in olivine using Raman spectroscopy, Am. Mineral., 99, 149–156, 2014.
