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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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Detalhes bibliográficos
Publicado no:Nat Commun
Main Authors: Agrusta, Roberto, van Hunen, Jeroen, Goes, Saskia
Formato: Artigo
Idioma:Inglês
Publicado em: Nature Publishing Group UK 2018
Assuntos:
Acesso em linha: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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