Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma

Descripción del Articulo

21 p.
Detalles Bibliográficos
Autores: Rousse, Sonia, Gilder, Stuart A., Farber, Daniel L., McNulty, Brendan A., Patriat, Philippe, Torres Bazán, Víctor Raúl, Sempere, Thierry
Formato: artículo
Fecha de Publicación:2003
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/630
Enlace del recurso:https://hdl.handle.net/20.500.12544/630
https://doi.org/10.1029/2003TC001508
Nivel de acceso:acceso abierto
Materia:Paleomagnetismo
Cinturón orogénico
Deformación
Magnetismo
Remanente
Orogenia andina
Subducción
Tectónica de placas
Placa de Nazca
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dc.title.es_PE.fl_str_mv Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
title Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
spellingShingle Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
Rousse, Sonia
Paleomagnetismo
Cinturón orogénico
Deformación
Magnetismo
Remanente
Orogenia andina
Subducción
Tectónica de placas
Placa de Nazca
title_short Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
title_full Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
title_fullStr Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
title_full_unstemmed Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
title_sort Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
author Rousse, Sonia
author_facet Rousse, Sonia
Gilder, Stuart A.
Farber, Daniel L.
McNulty, Brendan A.
Patriat, Philippe
Torres Bazán, Víctor Raúl
Sempere, Thierry
author_role author
author2 Gilder, Stuart A.
Farber, Daniel L.
McNulty, Brendan A.
Patriat, Philippe
Torres Bazán, Víctor Raúl
Sempere, Thierry
author2_role author
author
author
author
author
author
dc.contributor.author.fl_str_mv Rousse, Sonia
Gilder, Stuart A.
Farber, Daniel L.
McNulty, Brendan A.
Patriat, Philippe
Torres Bazán, Víctor Raúl
Sempere, Thierry
dc.subject.es_PE.fl_str_mv Paleomagnetismo
Cinturón orogénico
Deformación
Magnetismo
Remanente
Orogenia andina
Subducción
Tectónica de placas
Placa de Nazca
topic Paleomagnetismo
Cinturón orogénico
Deformación
Magnetismo
Remanente
Orogenia andina
Subducción
Tectónica de placas
Placa de Nazca
description 21 p.
publishDate 2003
dc.date.accessioned.none.fl_str_mv 2017-10-17T22:26:11Z
dc.date.available.none.fl_str_mv 2017-10-17T22:26:11Z
dc.date.issued.fl_str_mv 2003-09
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/article
format article
dc.identifier.citation.es_PE.fl_str_mv Rousse, S.; Gilder,S. A.; Farber, D. L.; McNulty, B. A.; Patriat, P.; Torres, V. & Sempere, T. (2003) - Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma. Tectonics, 22 (5): 21 p. doi: 10.1029/2003TC001508.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/630
dc.identifier.doi.none.fl_str_mv https://doi.org/10.1029/2003TC001508
dc.identifier.journal.es_PE.fl_str_mv Tectonics
dc.identifier.bibliographicCitation.es_PE.fl_str_mv Tectonics, v. 22, n. 5, 2003.
identifier_str_mv Rousse, S.; Gilder,S. A.; Farber, D. L.; McNulty, B. A.; Patriat, P.; Torres, V. & Sempere, T. (2003) - Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma. Tectonics, 22 (5): 21 p. doi: 10.1029/2003TC001508.
Tectonics
Tectonics, v. 22, n. 5, 2003.
url https://hdl.handle.net/20.500.12544/630
https://doi.org/10.1029/2003TC001508
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.relation.ispartof.none.fl_str_mv urn:issn:0278-7407
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
eu_rights_str_mv openAccess
dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Andes
Cajabamba
Cajamarca
Ica
Pisco
Nazca
Perú
Sudámerica
dc.coverage.temporal.none.fl_str_mv Cenozoico
Neógeno
Paleógeno
dc.publisher.es_PE.fl_str_mv John Wiley & Sons
dc.publisher.country.es_PE.fl_str_mv US
dc.source.es_PE.fl_str_mv Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
dc.source.none.fl_str_mv reponame:INGEMMET-Institucional
instname:Instituto Geológico, Minero y Metalúrgico
instacron:INGEMMET
instname_str Instituto Geológico, Minero y Metalúrgico
instacron_str INGEMMET
institution INGEMMET
reponame_str INGEMMET-Institucional
collection INGEMMET-Institucional
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spelling Rousse, SoniaGilder, Stuart A.Farber, Daniel L.McNulty, Brendan A.Patriat, PhilippeTorres Bazán, Víctor RaúlSempere, ThierryAndesCajabambaCajamarcaIcaPiscoNazcaPerúSudámericaCenozoicoNeógenoPaleógeno2017-10-17T22:26:11Z2017-10-17T22:26:11Z2003-09Rousse, S.; Gilder,S. A.; Farber, D. L.; McNulty, B. A.; Patriat, P.; Torres, V. & Sempere, T. (2003) - Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma. Tectonics, 22 (5): 21 p. doi: 10.1029/2003TC001508.https://hdl.handle.net/20.500.12544/630https://doi.org/10.1029/2003TC001508TectonicsTectonics, v. 22, n. 5, 2003.21 p.We report paleomagnetic data from 73 sites (628 samples) of upper Oligocene to Pliocene rocks from central and northern Peru. The data indicate that the Subandean Zone has not experienced vertical axis rotation since the upper Oligocene, whereas the coast and the Western Cordillera record a coherent pattern of counterclockwise rotations emplaced in the last 10 Ma. This pattern can best be explained by two competing hypotheses: (1) a propagation in rotations from the Bolivian Orocline toward the north or (2) a more punctual and widespread event linked to subduction of the Nazca Ridge that caused the rotations. On the basis of the time-space relationship of paleomagnetic rotations, deformation, magmatism and Nazca-South America plate convergence, the latter appears more likely. Moreover, because the rotations north of the Abancay deflection (~15.5°S) are synchronous with deformation and exhumation, they indicate that major mountain building in the Peruvian Andes has occurred since 10 Ma. Finally, we suggest that a succession of aseismic ridge subduction events played an important role in shaping the modern topography of the Andean chain.Peer reviewedapplication/pdfengJohn Wiley & SonsUSurn:issn:0278-7407info:eu-repo/semantics/openAccessRepositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETPaleomagnetismoCinturón orogénicoDeformaciónMagnetismoRemanenteOrogenia andinaSubducciónTectónica de placasPlaca de NazcaPaleomagnetic tracking of mountain building in the Peruvian Andes since 10 Mainfo:eu-repo/semantics/articleGeocienciasORIGINALRousse-Paleomagnetic tracking.pdfRousse-Paleomagnetic tracking.pdfArtículoapplication/pdf4147262https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/630/5/Rousse-Paleomagnetic%20tracking.pdff28845dacfe2e9d932ac7e992e96240dMD55LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/630/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52THUMBNAILRousse-Paleomagnetic tracking.pdf.jpgRousse-Paleomagnetic tracking.pdf.jpgGenerated Thumbnailimage/jpeg26739https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/630/4/Rousse-Paleomagnetic%20tracking.pdf.jpg1f5a827acc4f158330262af95ce1d025MD54TEXTRousse-Paleomagnetic tracking.pdf.txtRousse-Paleomagnetic tracking.pdf.txtExtracted texttext/plain98242https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/630/3/Rousse-Paleomagnetic%20tracking.pdf.txtc70c2ab55d0027a2dc74d4c599272034MD5320.500.12544/630oai:repositorio.ingemmet.gob.pe:20.500.12544/6302022-04-06 11:23:47.311Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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Paleomagnetic tracking of mountain building in the Peruvian Andes since 10 Ma
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