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Strong plates enhance mantle mixing in early Earth
In the present-day Earth, some subducting plates (slabs) are flattening above the upper–lower mantle boundary at ~670 km depth, whereas others go through, indicating a mode between layered and whole-mantle convection. Previous models predicted that in a few hundred degree hotter early Earth, convect...
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| Publicat a: | Nat Commun |
|---|---|
| Autors principals: | , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2018
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6045636/ https://ncbi.nlm.nih.gov/pubmed/30006629 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-05194-5 |
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