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Horizontal mantle flow controls subduction dynamics
It is generally accepted that subduction is driven by downgoing-plate negative buoyancy. Yet plate age –the main control on buoyancy– exhibits little correlation with most of the present-day subduction velocities and slab dips. “West”-directed subduction zones are on average steeper (~65°) than “Eas...
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| Publicado no: | Sci Rep |
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| 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/PMC5548891/ https://ncbi.nlm.nih.gov/pubmed/28790325 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-017-06551-y |
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