Crustal seismicity in the intra-arc region of Southern Andes (38°-40°S): insights of the Liquiñe-Ofqui Fault System and transverse-to-the-orogen fault systems

dc.date.accessioned2019-03-27T15:56:50Z
dc.date.accessioned2022-10-18T22:07:08Z
dc.date.available2019-03-27T15:56:50Z
dc.date.available2022-10-18T22:07:08Z
dc.date.created2019-03-27T15:56:50Z
dc.date.issued2016
dc.identifierhttp://hdl.handle.net/10533/233624
dc.identifier1141139
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4464981
dc.description.abstractSignificant tectonic activity takes place along intra-arc regions, being interrelated with volcanism, rock composition and landscape development. In the Southern Andes volcanic zone, little is known about the nature of crustal seismicity and its interplay
dc.languageeng
dc.relation9°
dc.relationinfo:eu-repo/grantAgreement/Fondecyt/1141139
dc.relationCities on Volcanoes
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titleCrustal seismicity in the intra-arc region of Southern Andes (38°-40°S): insights of the Liquiñe-Ofqui Fault System and transverse-to-the-orogen fault systems
dc.typePonencia


Este ítem pertenece a la siguiente institución