Cargando...

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...

Descrición completa

Gardado en:
Detalles Bibliográficos
Publicado en:Nat Commun
Main Authors: Xie, Longjian, Yoneda, Akira, Yamazaki, Daisuke, Manthilake, Geeth, Higo, Yuji, Tange, Yoshinori, Guignot, Nicolas, King, Andrew, Scheel, Mario, Andrault, Denis
Formato: Artigo
Idioma:Inglês
Publicado: Nature Publishing Group UK 2020
Assuntos:
Acceso en liña:https://ncbi.nlm.nih.gov/pmc/articles/PMC6987212/
https://ncbi.nlm.nih.gov/pubmed/31992697
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-14071-8
Tags: Engadir etiqueta
Sen Etiquetas, Sexa o primeiro en etiquetar este rexistro!