Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip

Article

Abstract: At subduction zones, transient aseismic slip occurs either as afterslip following a large earthquake

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Autores:

Cubas N., Jean Mathieu Nocquet, Patricia A. Mothes, Paul Jarrin, Plain M., Rolandone F., Sandro Vaca, Stephen Hernández, Vallée M., Yvonne Font

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