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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...
| Autores principales: | , , , , , , , , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
| Publicado: |
Nature Publishing Group UK
2020
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| Materias: | |
| 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 |