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Slow slip events in the roots of the San Andreas fault
Episodic tremor and accompanying slow slip are observed at the down-dip edge of subduction seismogenic zones. While tremors are the seismic signature of this phenomenon, they correspond to a small fraction of the moment released; thus, the associated fault slip can be quantified only by geodetic obs...
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| Publicado no: | Sci Adv |
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| Main Authors: | , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
American Association for the Advancement of Science
2019
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6374109/ https://ncbi.nlm.nih.gov/pubmed/30788438 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aav3274 |
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