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Systematic deficiency of aftershocks in areas of high coseismic slip for large subduction zone earthquakes
Fault slip during plate boundary earthquakes releases a portion of the shear stress accumulated due to frictional resistance to relative plate motions. Investigation of 101 large [moment magnitude (M(w)) ≥ 7] subduction zone plate boundary mainshocks with consistently determined coseismic slip distr...
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| Publicado no: | Sci Adv |
|---|---|
| Main Authors: | , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2018
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC5817929/ https://ncbi.nlm.nih.gov/pubmed/29487902 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aao3225 |
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