The lithosphere of Southern Peru: A result of the accretion of allochthonous blocks during the Mesoproterozoic

dc.creatorCarlotto Caillaux, Víctor Santiago
dc.creatorCárdenas Roque, José Dionicio
dc.creatorCarlier, Gabriel
dc.date.accessioned2022-04-22T16:55:33Z
dc.date.accessioned2022-10-27T15:37:23Z
dc.date.available2022-04-22T16:55:33Z
dc.date.available2022-10-27T15:37:23Z
dc.date.created2022-04-22T16:55:33Z
dc.date.issued2008
dc.identifierCarlotto, V.; Cárdenas, J. & Carlier, G. (2008). The lithosphere of Southern Peru: A result of the accretion of allochthonous blocks during the Mesoproterozoic. En: International Symposium on Andean Geodynamics, 7. Nice, 2008. Extended abstracts. Paris: IRD Éditions, p. 105-108.
dc.identifierhttps://hdl.handle.net/20.500.12544/3809
dc.identifier7th International Symposium on Andean Geodynamics (ISAG 2008, Nice), 2-4 September, 2008, Extended Abstracts.
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/4906651
dc.description.abstractSouthern Peru exhibits different juxtaposed structural blocks. These blocks have a distinct sedimentary, tectonic and magmatic evolution. They are bounded by complex, mainly NW-SE fault systems, locally marked by Cenozoic and Mesozoic magmatic units. The specific Mesozoic and Cenozoic geologic evolution of each structural block is ascribed to the high heterogeneity of the southern Peruvian depth lithosphere. This lithosphere results from the accretion of different lithospheric blocks during Laurentia-Amazonia collision at around 1000 Ma.
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.subjectAcreción
dc.subjectLitósfera
dc.subjectTerrenos alóctonos
dc.titleThe lithosphere of Southern Peru: A result of the accretion of allochthonous blocks during the Mesoproterozoic
dc.typeActas de congresos


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