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

Descripción del Articulo

Fault 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 depo...

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Detalles Bibliográficos
Autores: Flores, Alexander, Acosta Ale, Jorge Gilberto, Bedoya Jaén, Conrado, Sempere, Thierry
Formato: objeto de conferencia
Fecha de Publicación:2005
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/3799
Enlace del recurso:https://hdl.handle.net/20.500.12544/3799
Nivel de acceso:acceso abierto
Materia:Tectónica
Sedimentación
Sistema de fallas
Control estructural
Deformación
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
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dc.title.es_PE.fl_str_mv Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
title Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
spellingShingle Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
Flores, Alexander
Tectónica
Sedimentación
Sistema de fallas
Control estructural
Deformación
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
title_short Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
title_full Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
title_fullStr Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
title_full_unstemmed Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
title_sort Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
author Flores, Alexander
author_facet Flores, Alexander
Acosta Ale, Jorge Gilberto
Bedoya Jaén, Conrado
Sempere, Thierry
author_role author
author2 Acosta Ale, Jorge Gilberto
Bedoya Jaén, Conrado
Sempere, Thierry
author2_role author
author
author
dc.contributor.author.fl_str_mv Flores, Alexander
Acosta Ale, Jorge Gilberto
Bedoya Jaén, Conrado
Sempere, Thierry
dc.subject.es_PE.fl_str_mv Tectónica
Sedimentación
Sistema de fallas
Control estructural
Deformación
topic Tectónica
Sedimentación
Sistema de fallas
Control estructural
Deformación
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
dc.subject.ocde.es_PE.fl_str_mv http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
description Fault 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.
publishDate 2005
dc.date.accessioned.none.fl_str_mv 2022-04-22T16:24:40Z
dc.date.available.none.fl_str_mv 2022-04-22T16:24:40Z
dc.date.issued.fl_str_mv 2005
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dc.identifier.citation.es_PE.fl_str_mv Flores, 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.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/3799
dc.identifier.bibliographicCitation.es_PE.fl_str_mv 6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), 12-14 September, 2005, Extended Abstracts.
identifier_str_mv Flores, 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.
6th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), 12-14 September, 2005, Extended Abstracts.
url https://hdl.handle.net/20.500.12544/3799
dc.language.iso.es_PE.fl_str_mv eng
language eng
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
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eu_rights_str_mv openAccess
rights_invalid_str_mv https://creativecommons.org/licenses/by-nc-nd/4.0/deed.es
dc.format.es_PE.fl_str_mv application/pdf
dc.format.extent.es_PE.fl_str_mv 4 páginas
dc.coverage.spatial.es_PE.fl_str_mv Tacna
Perú
dc.publisher.es_PE.fl_str_mv IRD Éditions
dc.publisher.country.es_PE.fl_str_mv FRA
dc.source.es_PE.fl_str_mv Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
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spelling Flores, AlexanderAcosta Ale, Jorge GilbertoBedoya Jaén, ConradoSempere, ThierryTacnaPerú2022-04-22T16:24:40Z2022-04-22T16:24:40Z2005Flores, 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.https://hdl.handle.net/20.500.12544/37996th International Symposium on Andean Geodynamics (ISAG 2005, Barcelona), 12-14 September, 2005, Extended Abstracts.Fault 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.application/pdf4 páginasengIRD ÉditionsFRAinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-nd/4.0/deed.esRepositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETTectónicaSedimentaciónSistema de fallasControl estructuralDeformaciónhttp://purl.org/pe-repo/ocde/ford#1.05.00http://purl.org/pe-repo/ocde/ford#1.05.06Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)info:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionORIGINALFlores-Oligocene_Neogene_tectonics-Peru.pdfFlores-Oligocene_Neogene_tectonics-Peru.pdfArtículo de congresoapplication/pdf130099https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3799/1/Flores-Oligocene_Neogene_tectonics-Peru.pdf9726a7ece685f53d31f1bddf51a891e0MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3799/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52TEXTFlores-Oligocene_Neogene_tectonics-Peru.pdf.txtFlores-Oligocene_Neogene_tectonics-Peru.pdf.txtExtracted texttext/plain10673https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3799/3/Flores-Oligocene_Neogene_tectonics-Peru.pdf.txtb35338a2273271578c48a5daafd2537aMD53THUMBNAILFlores-Oligocene_Neogene_tectonics-Peru.pdf.jpgFlores-Oligocene_Neogene_tectonics-Peru.pdf.jpgGenerated Thumbnailimage/jpeg16591https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3799/6/Flores-Oligocene_Neogene_tectonics-Peru.pdf.jpg4a1a69e26199f399fb29f3fa9a975baeMD5620.500.12544/3799oai:repositorio.ingemmet.gob.pe:20.500.12544/37992022-04-22 14:00:23.303Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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Oligocene-Neogene tectonics and sedimentation in the forearc of southern Peru, Tacna area (17.5°-18.5°5)
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