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Mantle updrafts and mechanisms of oceanic volcanism
Convection in an isolated planet is characterized by narrow downwellings and broad updrafts—consequences of Archimedes’ principle, the cooling required by the second law of thermodynamics, and the effect of compression on material properties. A mature cooling planet with a conductive low-viscosity c...
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| Autors principals: | , |
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| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
National Academy of Sciences
2014
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4205608/ https://ncbi.nlm.nih.gov/pubmed/25201992 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1410229111 |
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