Oxygen-rich melt in deep magma oceans

被引：0
|
作者：
Gaillard, Fabrice [1 ]
机构：
[1] Univ Orleans, Inst Sci Terre Orleans, CNRS, BRGM, Orleans, France
来源：
NATURE GEOSCIENCE | 2023年 / 16卷 / 05期
关键词：
OXIDATION-STATE; TERRESTRIAL; ACCRETION;
D O I：
10.1038/s41561-023-01178-3
中图分类号：
P [天文学、地球科学];
学科分类号：
07 ;
摘要：
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.
引用
收藏
页码：392 / 393
页数：2
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