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...

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Udgivet i:Nat Commun
Main Authors: Rowe, Christie D., Lamothe, Kelsey, Rempe, Marieke, Andrews, Mark, Mitchell, Thomas M., Di Toro, Giulio, White, Joseph Clancy, Aretusini, Stefano
Format: Artigo
Sprog:Inglês
Udgivet: Nature Publishing Group UK 2019
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Article
Online adgang:https://ncbi.nlm.nih.gov/pmc/articles/PMC6338773/
https://ncbi.nlm.nih.gov/pubmed/30659201
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-018-08238-y
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