Dynamic friction and the origin of the complexity of earthquake sources.
We study a simple antiplane fault of finite length embedded in a homogeneous isotropic elastic solid to understand the origin of seismic source heterogeneity in the presence of nonlinear rate- and state-dependent friction. All the mechanical properties of the medium and friction are assumed homogene...
Uloženo v:
| Vydáno v: | Proc Natl Acad Sci U S A |
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| Hlavní autoři: | , |
| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
National Academy of Sciences
1996
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| Témata: | |
| On-line přístup: | https://ncbi.nlm.nih.govhttps://pmc.ncbi.nlm.nih.gov/articles/PMC39442/ https://ncbi.nlm.nih.govhttps://pubmed.ncbi.nlm.nih.gov/11607670/ https://ncbi.nlm.nih.govhttps://doi.org/10.1073/pnas.93.9.3819 |
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