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Earthquake swarms and slow slip on a sliver fault in the Mexican subduction zone
The Mexican subduction zone is an ideal location for studying subduction processes due to the short trench-to-coast distances that bring broad portions of the seismogenic and transition zones of the plate interface inland. Using a recently generated seismicity catalog from a local network in Oaxaca,...
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| Publicado no: | Proc Natl Acad Sci U S A |
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| Main Authors: | , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
National Academy of Sciences
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6462109/ https://ncbi.nlm.nih.gov/pubmed/30910959 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1814205116 |
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