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Earthquake lubrication and healing explained by amorphous nanosilica
During earthquake propagation, geologic faults lose their strength, then strengthen as slip slows and stops. Many slip-weakening mechanisms are active in the upper-mid crust, but healing is not always well-explained. Here we show that the distinct structure and rate-dependent properties of amorphous...
Autores principales: | Rowe, Christie D., Lamothe, Kelsey, Rempe, Marieke, Andrews, Mark, Mitchell, Thomas M., Di Toro, Giulio, White, Joseph Clancy, Aretusini, Stefano |
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Formato: | Online Artículo Texto |
Lenguaje: | English |
Publicado: |
Nature Publishing Group UK
2019
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Materias: | |
Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6338773/ https://www.ncbi.nlm.nih.gov/pubmed/30659201 http://dx.doi.org/10.1038/s41467-018-08238-y |
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