Caricamento...
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...
Salvato in:
| Pubblicato in: | Nat Commun |
|---|---|
| Autori principali: | , , , , , , |
| Natura: | Artigo |
| Lingua: | Inglês |
| Pubblicazione: |
Nature Publishing Group UK
2017
|
| Soggetti: | |
| Accesso online: | 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 |
| Tags: |
Aggiungi Tag
Nessun Tag, puoi essere il primo ad aggiungerne! !
|