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Shearing instabilities accompanying high-pressure phase transformations and the mechanics of deep earthquakes
Deep earthquakes have been a paradox since their discovery in the 1920s. The combined increase of pressure and temperature with depth precludes brittle failure or frictional sliding beyond a few tens of kilometers, yet earthquakes occur continually in subduction zones to ≈700 km. The expected healin...
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| Formato: | Artigo |
| Idioma: | Inglês |
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National Academy of Sciences
2007
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| Acceso en liña: | https://ncbi.nlm.nih.gov/pmc/articles/PMC1890459/ https://ncbi.nlm.nih.gov/pubmed/17468397 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.0608045104 |
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