Mostrar el registro sencillo del ítem

dc.contributor.author Nocquet, J.-M.
dc.contributor.author Villegas Lanza, Juan Carlos
dc.contributor.author Chlieh, M.
dc.contributor.author Mothes, P. A.
dc.contributor.author Rolandone, F.
dc.contributor.author Jarrin, P.
dc.contributor.author Cisneros, D.
dc.contributor.author Alvarado, A.
dc.contributor.author Audin, L.
dc.contributor.author Bondoux, F.
dc.contributor.author Martin, X.
dc.contributor.author Font, Y.
dc.contributor.author Régnier, M.
dc.contributor.author Vallée, M.
dc.contributor.author Tran, T.
dc.contributor.author Beauval, C.
dc.contributor.author Maguiña Mendoza, J.M.
dc.contributor.author Martinez, W.
dc.contributor.author Tavera, Hernando
dc.contributor.author Yepes, H.
dc.coverage.spatial Ecuador
dc.coverage.spatial Perú
dc.date.accessioned 2018-07-31T18:43:23Z
dc.date.available 2018-07-31T18:43:23Z
dc.date.issued 2014
dc.identifier.citation Nocquet, J-M., Villegas-Lanza, J. C., Chlieh, M., Mothes, P. A., Rolandone, F., Jarrin, P., . . . Yepes, H. (2014). Motion of continental slivers and creeping subduction in the northern andes.==$Nature Geoscience, 7$==(4), 287–291. https://doi.org/10.1038/ngeo2099 es_ES
dc.identifier.govdoc index-oti2018
dc.identifier.uri http://hdl.handle.net/20.500.12816/2141
dc.description.abstract Along the western margin of South America, plate convergence is accommodated by slip on the subduction interface and deformation of the overriding continent. In Chile, Bolivia, Ecuador and Colombia, continental deformation occurs mostly through the motion of discrete domains, hundreds to thousands of kilometres in scale. These continental slivers are wedged between the Nazca and stable South American plates. Here we use geodetic data to identify another large continental sliver in Peru that is about 300–400 km wide and 1,500 km long, which we call the Inca Sliver. We show that movement of the slivers parallel to the subduction trench is controlled by the obliquity of plate convergence and is linked to prominent features of the Andes Mountains. For example, the Altiplano is located at the boundary of converging slivers at the concave bend of the central Andes, and the extending Gulf of Guayaquil is located at the boundary of diverging slivers at the convex bend of the northern Andes. Motion of a few large continental slivers therefore controls the present-day deformation of nearly the entire Andes mountain range. We also show that a 1,000-km-long section of the plate interface in northern Peru and southern Ecuador slips predominantly aseismically, a behaviour that contrasts with the highly seismic neighbouring segments. The primary characteristics of this low-coupled segment are shared by ~20% of the subduction zones in the eastern Pacific Rim. es_ES
dc.format application/pdf es_ES
dc.language.iso eng es_ES
dc.publisher Nature Research es_ES
dc.relation.ispartof urn:issn:1752-0894
dc.rights info:eu-repo/semantics/closedAccess es_ES
dc.subject Seismology es_ES
dc.subject Tectonics es_ES
dc.subject Subduction es_ES
dc.title Motion of continental slivers and creeping subduction in the northern Andes es_ES
dc.type info:eu-repo/semantics/article es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.00 es_ES
dc.subject.ocde http://purl.org/pe-repo/ocde/ford#1.05.04 es_ES
dc.identifier.journal Nature Geoscience es_ES
dc.description.peer-review Por pares es_ES
dc.identifier.doi https://doi.org/10.1038/ngeo2099 es_ES

Thumbnail

 Bloqueado

Colecciones

Mostrar el registro sencillo del ítem