dc.contributorCembrano-Perasso, José Migue
dc.contributorPontificia Universidad Católica de Chile
dc.creatorStanton-Yonge Sesnic, Ashley
dc.date2019-05-14T21:40:33Z
dc.date2022-08-16T18:42:04Z
dc.date2019-05-14T21:40:33Z
dc.date2022-08-16T18:42:04Z
dc.date2016
dc.date.accessioned2023-08-22T11:02:00Z
dc.date.available2023-08-22T11:02:00Z
dc.identifier1141139
dc.identifierhttps://hdl.handle.net/10533/235600
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8342371
dc.descriptionObliquely convergent subduction margins develop trench-parallel faults shaping the regional architecture of orogenic belts and partitioning interplate deformation. However, transverse faults also are common along most orogenic belts, although have been la
dc.descriptionFONDECYT
dc.descriptionFONDECYT
dc.languageeng
dc.relationinstname: Conicyt
dc.relationreponame: Repositorio Digital RI2.0
dc.relationhttps://repositorio.uc.cl/bitstream/handle/11534/16840/000673942.pdf?sequence=1&isAllowed=y
dc.rightsinfo:eu-repo/semantics/openAccess
dc.rightsAttribution-NonCommercial-NoDerivs 3.0 Chile
dc.rightshttp://creativecommons.org/licenses/by-nc-nd/3.0/cl/
dc.subjectCiencias Naturales
dc.subjectCiencias de la Tierra y del Medio Ambiente
dc.titleTectonic Role Of Margin-Parallel And Margin-Transverse Faults During Oblique Subduction At The Southern Volcanic Zone Of The Andes
dc.typeTesis Magíster
dc.typeTesis Magíster
dc.typeinfo:eu-repo/semantics/masterThesis
dc.typeinfo:eu-repo/semantics/publishedVersion
dc.typeTesis


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