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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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| Published in: | Sci Adv |
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| Main Authors: | , , , , , |
| Format: | Artigo |
| Language: | Inglês |
| Published: |
American Association for the Advancement of Science
2016
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| Subjects: | |
| Online Access: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4928950/ https://ncbi.nlm.nih.gov/pubmed/27386548 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1600246 |
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