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From slow to fast faulting: recent challenges in earthquake fault mechanics
Faults—thin zones of highly localized shear deformation in the Earth—accommodate strain on a momentous range of dimensions (millimetres to hundreds of kilometres for major plate boundaries) and of time intervals (from fractions of seconds during earthquake slip, to years of slow, aseismic slip and m...
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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/PMC5580450/ https://ncbi.nlm.nih.gov/pubmed/28827428 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rsta.2016.0016 |
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