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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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| Gepubliceerd in: | Philos Trans A Math Phys Eng Sci |
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| Hoofdauteur: | |
| Formaat: | Artigo |
| Taal: | Inglês |
| Gepubliceerd in: |
The Royal Society Publishing
2017
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| Onderwerpen: | |
| Online toegang: | 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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