Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)

dc.creatorFlores, Alexander
dc.creatorAcosta Ale, Jorge Gilberto
dc.creatorBedoya Jaén, Conrado
dc.creatorSempere, Thierry
dc.date.accessioned2022-04-22T16:24:40Z
dc.date.accessioned2022-10-27T15:38:55Z
dc.date.available2022-04-22T16:24:40Z
dc.date.available2022-10-27T15:38:55Z
dc.date.created2022-04-22T16:24:40Z
dc.date.issued2005
dc.identifierFlores, A.; Acosta, J.; Bedoya, C. & Sempere, T. (2005). Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5). En: International Symposium on Andean Geodynamics, 6, Barcelona, 2005. Extended abstracts. Paris: IRD Éditions, p. 269-272.
dc.identifierhttps://hdl.handle.net/20.500.12544/3799
dc.identifier6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), 12-14 September, 2005, Extended Abstracts.
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4907500
dc.description.abstractFault systems observed in the southernmost Peruvian forearc (Tacna area) provide information on the structure of the inner Bolivian Orocline (Arica elbow). Here we present the characteristics of the main fault systems observed in the Tacna area, as well as evidences of structural control on the deposition of Upper Cenozoic units and regional geoforms. We propose a synthetic chronology of deformation.
dc.languageeng
dc.publisherIRD Éditions
dc.publisherFRA
dc.rightshttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
dc.rightsinfo:eu-repo/semantics/openAccess
dc.sourceRepositorio Institucional INGEMMET
dc.sourceInstituto Geológico, Minero y Metalúrgico – INGEMMET
dc.subjectTectónica
dc.subjectSedimentación
dc.subjectSistema de fallas
dc.subjectControl estructural
dc.subjectDeformación
dc.titleOligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
dc.typeActas de congresos


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