Forearc deformation along the peruvian margin and the effects of changes in subduction style: quantifying the rates of Quaternary deformation using in situ produced cosmogenic 10Be and 26Al.

dc.creatorHall, Sarah R.
dc.creatorFarber, Daniel L.
dc.creatorAudin, Laurence
dc.creatorMériaux, Anne-Sophie
dc.creatorTorres Bazán, Víctor Raúl
dc.date.accessioned2021-11-17T21:35:04Z
dc.date.accessioned2022-10-27T15:37:39Z
dc.date.available2021-11-17T21:35:04Z
dc.date.available2022-10-27T15:37:39Z
dc.date.created2021-11-17T21:35:04Z
dc.date.issued2004
dc.identifierHall, S.; Farber, D.; Audin, L.; Mériaux, A. & Torres, V. (2004) - Forearc deformation along the peruvian margin and the effects of changes in subduction style: quantifying the rates of Quaternary deformation using in situ produced cosmogenic 10Be and 26Al. En: Congreso Peruano de Geología, 12, Lima, 2004. Resúmenes extendidos. Lima: Sociedad Geológica del Perú, 4 p.
dc.identifierhttps://hdl.handle.net/20.500.12544/3472
dc.identifierXII Congreso Peruano de Geología, Lima, 2004. Resúmenes extendidos.
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4906812
dc.description.abstractThe Andes are one ofthe world's two highest mountain ranges and together wíth the westem cordillera of North America they forro an almost a continuous mountaín chain from the tip of Patagonia to the Alaskan peninsula. Common to all the cordillera of westem North and South America is the ín:fluence oflong-lived subduction. Indeed, the style of this subduction process has profoundly modified the margin of both continents. For example, following relatively normal subduction in the Jurassíc and the Cretaceous, the Laramide orogeny of North America is thought to have been produced from effects of extremely flat subduction.
dc.languagespa
dc.publisherSociedad Geológica del Perú
dc.publisherPE
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.subjectDeformación
dc.subjectIsótopos
dc.subjectMargen continental
dc.subjectSubducción
dc.subjectTectónica
dc.titleForearc deformation along the peruvian margin and the effects of changes in subduction style: quantifying the rates of Quaternary deformation using in situ produced cosmogenic 10Be and 26Al.
dc.typeActas de congresos


Este ítem pertenece a la siguiente institución