Please use this identifier to cite or link to this item: https://hdl.handle.net/20.500.12544/3809
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Carlotto Caillaux, Víctor Santiago
Cárdenas Roque, José Dionicio
Carlier, Gabriel
Altiplano
Macizo de Arequipa
Región Sur
Perú
2022-04-22T16:55:33Z
2022-04-22T16:55:33Z
2008
Carlotto, 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.
https://hdl.handle.net/20.500.12544/3809
Southern 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.
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4 páginas
eng
IRD Éditions
info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
Acreción
Litósfera
Terrenos alóctonos
The lithosphere of Southern Peru: A result of the accretion of allochthonous blocks during the Mesoproterozoic
info:eu-repo/semantics/conferenceObject
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
FRA
info:eu-repo/semantics/publishedVersion
7th International Symposium on Andean Geodynamics (ISAG 2008, Nice), 2-4 September, 2008, Extended Abstracts.

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