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Phase-transformation-induced lubrication of earthquake sliding
Frictional failure is not possible at depth in Earth, hence earthquakes deeper than 30–50 km cannot initiate by overcoming dry friction. Moreover, the frequency distribution of earthquakes with depth is bimodal, suggesting another change of mechanism at about 350 km. Here I suggest that the change a...
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| Publicado no: | Philos Trans A Math Phys Eng Sci |
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| Autor principal: | |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Royal Society Publishing
2017
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5580448/ https://ncbi.nlm.nih.gov/pubmed/28827426 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2016.0008 |
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