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Modeling fast and slow earthquakes at various scales
Earthquake sources represent dynamic rupture within rocky materials at depth and often can be modeled as propagating shear slip controlled by friction laws. These laws provide boundary conditions on fault planes embedded in elastic media. Recent developments in observation networks, laboratory exper...
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| Udgivet i: | Proc Jpn Acad Ser B Phys Biol Sci |
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| Hovedforfatter: | |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
The Japan Academy
2014
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4275565/ https://ncbi.nlm.nih.gov/pubmed/25311138 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.2183/pjab.90.259 |
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