Vertically Resolved Magma Ocean–Protoatmosphere Evolution: H2, H2O, CO2, CH4, CO, O2, and N2 as Primary Absorbers
The earliest atmospheres of rocky planets originate from extensive volatile release during magma ocean epochs that occur during assembly of the planet. These establish the initial distribution of the major volatile elements between different chemical reservoirs that subsequently evolve via geologica...
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Published in | Journal of geophysical research. Planets Vol. 126; no. 2 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
01.02.2021
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Subjects | |
Online Access | Get full text |
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