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Areas prone to slow slip events impede earthquake rupture propagation and promote afterslip
ArticleAbstract: At subduction zones, transient aseismic slip occurs either as afterslip following a large earthquakePalabras claves:Autores:Cubas N., Jean Mathieu Nocquet, Patricia A. Mothes, Paul Jarrin, Plain M., Rolandone F., Sandro Vaca, Stephen Hernández, Vallée M., Yvonne FontFuentes:googlescopusEvidences of Surface Rupture Associated With a Low-Magnitude (M<inf>w</inf>5.0) Shallow Earthquake in the Ecuadorian Andes
ArticleAbstract: This study analyzes surface displacements generated by a low-magnitude crustal earthquake in the EcuPalabras claves:ECUADOR, InSAR, shallow earthquake, surface rutpureAutores:Alexandra P. Alvarado, Audin L., Baize S., Champenois J., Ekstöm G., Espín P.A., Jomard H., Vallée M.Fuentes:googlescopus