Formation of bridgmanite-enriched layer at the top lower-mantle during magma ocean solidification

Thermochemical heterogeneities detected today in the Earth’s mantle could arise from ongoing partial melting in different mantle regions. A major open question, however, is the level of chemical stratification inherited from an early magma-ocean (MO) solidification. Here we show that the MO crystall...

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Detalles Bibliográficos
Autores principales: Xie, Longjian, Yoneda, Akira, Yamazaki, Daisuke, Manthilake, Geeth, Higo, Yuji, Tange, Yoshinori, Guignot, Nicolas, King, Andrew, Scheel, Mario, Andrault, Denis
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2020
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6987212/
https://www.ncbi.nlm.nih.gov/pubmed/31992697
http://dx.doi.org/10.1038/s41467-019-14071-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6987212/
https://www.ncbi.nlm.nih.gov/pubmed/31992697
http://dx.doi.org/10.1038/s41467-019-14071-8

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