Ultra-thin clay layers facilitate seismic slip in carbonate faults

Abstract Many earthquakes propagate up to the Earth’s surface producing surface ruptures. Seismic slip propagation is facilitated by along-fault low dynamic frictional resistance, which is controlled by a number of physico-chemical lubrication mechanisms. In particular, rotary shear experiments cond...

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Autores principales: Luca Smeraglia, Andrea Billi, Eugenio Carminati, Andrea Cavallo, Giulio Di Toro, Elena Spagnuolo, Federico Zorzi
Formato: article
Lenguaje:EN
Publicado: Nature Portfolio 2017
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Acceso en línea:https://doaj.org/article/9281ea0ae337402d9d8c227324445878
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