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A mixed seismic-aseismic stress release episode in the Andean subduction zone
ArticleAbstract: In subduction zones, stress is released by earthquakes and transient aseismic slip. The latter fallsPalabras claves:Autores:Bondoux F., Chlieh M., Jean Mathieu Nocquet, Martin X., Rolandone F., Tavera H., Tran T., Vallée M., Villegas-Lanza J.C.Fuentes:scopusMotion of continental slivers and creeping subduction in the northern Andes
ArticleAbstract: Along the western margin of South America, plate convergence is accommodated by slip on the subductiPalabras claves:Autores:Alexandra P. Alvarado, Audin L., Beauval C., Bondoux F., Chlieh M., Cisneros D., Hugo Yepes, Jean Mathieu Nocquet, Maguiña Mendoza J.M., Martin X., Martinez W., Patricia A. Mothes, Paul Jarrin, Regnier M.M., Rolandone F., Tavera H., Tran T., Vallée M., Villegas-Lanza J.C., Yvonne FontFuentes:googlescopusPresent-day uplift of the western Alps
ArticleAbstract: Collisional mountain belts grow as a consequence of continental plate convergence and eventually disPalabras claves:Autores:Baize S., Chéry J., Cushing M., Jean Mathieu Nocquet, Jouanne F., Lenôtre N., Masson F., Sue C., Tran T., Van Der Beek P.A., Vernant P., Walpersdorf A.Fuentes:scopus