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Episodic creep events on the San Andreas Fault caused by pore-pressure variations
Recent seismic and geodetic observations indicate that interseismic creep rate varies in both time and space. The spatial extent of creep pinpoints locked asperities, while its temporary accelerations, known as slow-slip events, may trigger earthquakes. Although the conditions promoting fault creep...
| Autores principales: | , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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2018
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| Materias: | |
| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6008793/ https://www.ncbi.nlm.nih.gov/pubmed/29937919 http://dx.doi.org/10.1038/s41561-018-0160-2 |