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Experimental evidence supporting a global melt layer at the base of the Earth’s upper mantle
The low-velocity layer (LVL) atop the 410-km discontinuity has been widely attributed to dehydration melting. In this study, we experimentally reproduced the wadsleyite-to-olivine phase transformation in the upwelling mantle across the 410-km discontinuity and investigated in situ the sound wave vel...
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| Publicado no: | Nat Commun |
|---|---|
| Main Authors: | , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group UK
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5736617/ https://ncbi.nlm.nih.gov/pubmed/29259159 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-017-02275-9 |
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