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...

Descripción completa

Detalles Bibliográficos
Autores principales: Rowe, Christie D., Lamothe, Kelsey, Rempe, Marieke, Andrews, Mark, Mitchell, Thomas M., Di Toro, Giulio, White, Joseph Clancy, Aretusini, Stefano
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2019
Materias:
Article
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

Internet

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

Ejemplares similares