Exploring the shallow structure of the San Ramón thrust fault in Santiago, Chile (∼33.5° S), using active seismic and electric methods

dc.date.accessioned2020-03-11T20:26:35Z
dc.date.accessioned2022-10-18T22:41:16Z
dc.date.available2020-03-11T20:26:35Z
dc.date.available2022-10-18T22:41:16Z
dc.date.created2020-03-11T20:26:35Z
dc.date.issued2014
dc.identifierhttp://hdl.handle.net/10533/238064
dc.identifier15090013
dc.identifierWOS:000347545800019
dc.identifierno scielo
dc.identifiereid=2-s2.0-84940316543
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4469403
dc.description.abstractThe crustal-scale west-vergent San Ramón thrust fault system at the foot of the main Andean Cordillera in central Chile is a geologically active structure with Quaternary manifestations of complex surface rupture along fault segments in the eastern bor- d
dc.languageeng
dc.relationhttps://doi.org/10.5194/se-5-837-2014
dc.relation10.5194/se-5-837-2014
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAtribución-NoComercial-SinDerivadas 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.titleExploring the shallow structure of the San Ramón thrust fault in Santiago, Chile (∼33.5° S), using active seismic and electric methods
dc.typeArticulo


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