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Reaction-induced rheological weakening enables oceanic plate subduction
Earth is the only terrestrial planet in our solar system where an oceanic plate subducts beneath an overriding plate. Although the initiation of plate subduction requires extremely weak boundaries between strong plates, the way in which oceanic mantle rheologically weakens remains unknown. Here we s...
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| Vydáno v: | Nat Commun |
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| Hlavní autoři: | , , , , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Publishing Group
2016
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5007449/ https://ncbi.nlm.nih.gov/pubmed/27562366 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms12550 |
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