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...

Disgrifiad llawn

Wedi'i Gadw mewn:
Manylion Llyfryddiaeth
Cyhoeddwyd yn:Nat Commun
Prif Awduron: Rowe, Christie D., Lamothe, Kelsey, Rempe, Marieke, Andrews, Mark, Mitchell, Thomas M., Di Toro, Giulio, White, Joseph Clancy, Aretusini, Stefano
Fformat: Artigo
Iaith:Inglês
Cyhoeddwyd: Nature Publishing Group UK 2019
Pynciau:
Article
Mynediad Ar-lein: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
Tagiau: Ychwanegu Tag
Dim Tagiau, Byddwch y cyntaf i dagio'r cofnod hwn!

Eitemau Tebyg