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dc.contributor.advisorMitchell, Thomas
dc.creatorPearce, Rebecca
dc.date.accessioned2019-05-14T21:40:33Z
dc.date.available2019-05-14T21:40:33Z
dc.date.issued2015
dc.identifier.urihttp://hdl.handle.net/10533/235605
dc.description.abstractIn a tectonic regime dominated by North-South oriented convergent stresses, margin oblique lineaments in the main cordillera of the Chilean Andes are theorized to significantly contribute to the dynamic evolution of this mountain belt as hydrothermal and
dc.language.isoeng
dc.relationinstname: Conicyt
dc.relationreponame: Repositorio Digital RI2.0
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.titleInvestigating the Gravity Signatures of the Margin-Oblique Deep Seated Andean Faults in the Rio Teno Region of the Transitional Southern Volcanic Zone, Chile
dc.typeTesis Magíster
dc.typeTesis Magíster
dc.contributor.institutionUniversity College London
dc.identifier.folio1141139
dc.country.isogbr
dc.description.conicytprogramFONDECYT
dc.type.driverinfo:eu-repo/semantics/masterThesis
dc.description.shortconicytprogramFONDECYT
dc.type.tesisTesis
dc.subject.oecd1nCiencias Naturales
dc.subject.oecd2nCiencias de la Tierra y del Medio Ambiente
dc.type.openaireinfo:eu-repo/semantics/publishedVersion


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