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...
Gardado en:
| Publicado en: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , , , , |
| 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!
|