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Oxygen-rich melt in deep magma oceans
Gaillard, F. (2023). Oxygen-rich melt in deep magma oceans. Nature Geoscience 16(5): 392-393. https://dx.doi.org/10.1038/s41561-023-01178-3
In: Nature Geoscience. Nature Publishing Group: London. ISSN 1752-0894; e-ISSN 1752-0908, meer
Is gerelateerd aan:
Kuwahara, H.; Nakada, R.; Kadoya, S.; Yoshino, T.; Irifune, T. (2023). Hadean mantle oxidation inferred from melting of peridotite under lower-mantle conditions. Nature Geoscience 16(5): 461-465. https://dx.doi.org/10.1038/s41561-023-01169-4, meer
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  • Gaillard, F.
Abstract
    High pressures may have enabled ferric iron-rich silicate melts to coexist with iron metal near the base of magma oceans early in the history of large rocky planets like Earth. This suggests a relatively oxygen-rich atmosphere during the late stages of core formation on these planets.
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