Experimental evidence supports mantle partial melting in the asthenosphere

The low-velocity zone (LVZ) is a persistent seismic feature in a broad range of geological contexts. It coincides in depth with the asthenosphere, a mantle region of lowered viscosity that may be essential to enabling plate motions. The LVZ has been proposed to originate from either partial melting...

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Detalles Bibliográficos
Autores principales: Chantel, Julien, Manthilake, Geeth, Andrault, Denis, Novella, Davide, Yu, Tony, Wang, Yanbin
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2016
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4928950/
https://www.ncbi.nlm.nih.gov/pubmed/27386548
http://dx.doi.org/10.1126/sciadv.1600246

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4928950/
https://www.ncbi.nlm.nih.gov/pubmed/27386548
http://dx.doi.org/10.1126/sciadv.1600246

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