Timescales of chemical equilibrium between the convecting solid mantle and over- and underlying magma oceans
<p>After accretion and formation, terrestrial planets go through at least one magma ocean episode. As the magma ocean crystallises, it creates the first layer of solid rocky mantle. Two different scenarios of magma ocean crystallisation involve that the solid mantle either (1) first appears at...
| Main Authors: | , , , , , , |
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| Formato: | Artigo |
| Idioma: | English |
| Publicado em: |
Copernicus Publications
2021-02-01
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| Colecção: | Solid Earth |
| Acesso em linha: | https://se.copernicus.org/articles/12/421/2021/se-12-421-2021.pdf |