K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru
Descripción del Articulo
K-Ar ages were determined on 30 Andean volcanic rocks from southern Peru, most of which were considered to belong to the Barroso Group of Quaternary in age. The results have revealed, however, that their ages range from late Miocene to recent (7.2 to less than 0.03 Ma). This indicates that the Barro...
Autores: | , |
---|---|
Formato: | artículo |
Fecha de Publicación: | 1984 |
Institución: | Instituto Geológico, Minero y Metalúrgico |
Repositorio: | INGEMMET-Institucional |
Lenguaje: | inglés |
OAI Identifier: | oai:repositorio.ingemmet.gob.pe:20.500.12544/1505 |
Enlace del recurso: | https://hdl.handle.net/20.500.12544/1505 https://doi.org/10.2343/geochemj.18.233 |
Nivel de acceso: | acceso abierto |
Materia: | Datación K-Ar Geocronología Rocas volcánicas Grupo Sencca Grupo Tacaza |
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dc.title.es_PE.fl_str_mv |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
title |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
spellingShingle |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru Kaneoka, Ichiro Datación K-Ar Geocronología Rocas volcánicas Grupo Sencca Grupo Tacaza |
title_short |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
title_full |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
title_fullStr |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
title_full_unstemmed |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
title_sort |
K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru |
author |
Kaneoka, Ichiro |
author_facet |
Kaneoka, Ichiro Guevara Rosillo, Carlos |
author_role |
author |
author2 |
Guevara Rosillo, Carlos |
author2_role |
author |
dc.contributor.author.fl_str_mv |
Kaneoka, Ichiro Guevara Rosillo, Carlos |
dc.subject.es_PE.fl_str_mv |
Datación K-Ar Geocronología Rocas volcánicas Grupo Sencca Grupo Tacaza |
topic |
Datación K-Ar Geocronología Rocas volcánicas Grupo Sencca Grupo Tacaza |
description |
K-Ar ages were determined on 30 Andean volcanic rocks from southern Peru, most of which were considered to belong to the Barroso Group of Quaternary in age. The results have revealed, however, that their ages range from late Miocene to recent (7.2 to less than 0.03 Ma). This indicates that the Barroso Group samples might include much wider age ranges than had been assigned. Relatively young volcanic activity of late Quaternary is apparently restricted in the northwestern part including the vicinity of Arequipa in the investigated area. The main volcanic activity in the southwestern part seem to have almost ended by early Pleistocene. The shoshonitic rocks which are located around the Puno area probably extruded about 6Ma ago in a relatively short period of less than a few hundred thousand years. |
publishDate |
1984 |
dc.date.accessioned.none.fl_str_mv |
2018-06-22T21:26:53Z |
dc.date.available.none.fl_str_mv |
2018-06-22T21:26:53Z |
dc.date.issued.fl_str_mv |
1984 |
dc.type.es_PE.fl_str_mv |
info:eu-repo/semantics/article |
format |
article |
dc.identifier.citation.es_PE.fl_str_mv |
Kaneoka, I. & Guevara, C. (1984) - K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru. Geochemical Journal, 18(5): 233–239. Doi: 10.2343/geochemj.18.233 |
dc.identifier.uri.none.fl_str_mv |
https://hdl.handle.net/20.500.12544/1505 |
dc.identifier.doi.none.fl_str_mv |
https://doi.org/10.2343/geochemj.18.233 |
dc.identifier.journal.es_PE.fl_str_mv |
Geochemical Journal |
dc.identifier.bibliographicCitation.es_PE.fl_str_mv |
Geochemical Journal, 18(5): 233–239, 1984 |
identifier_str_mv |
Kaneoka, I. & Guevara, C. (1984) - K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru. Geochemical Journal, 18(5): 233–239. Doi: 10.2343/geochemj.18.233 Geochemical Journal Geochemical Journal, 18(5): 233–239, 1984 |
url |
https://hdl.handle.net/20.500.12544/1505 https://doi.org/10.2343/geochemj.18.233 |
dc.language.iso.es_PE.fl_str_mv |
eng |
language |
eng |
dc.relation.ispartof.none.fl_str_mv |
urn:issn:1880-5973 |
dc.rights.es_PE.fl_str_mv |
info:eu-repo/semantics/openAccess |
dc.rights.uri.es_PE.fl_str_mv |
https://creativecommons.org/licenses/by-sa/4.0/ |
eu_rights_str_mv |
openAccess |
rights_invalid_str_mv |
https://creativecommons.org/licenses/by-sa/4.0/ |
dc.format.es_PE.fl_str_mv |
application/pdf |
dc.coverage.spatial.es_PE.fl_str_mv |
Andes Arequipa Puno Perú |
dc.coverage.temporal.none.fl_str_mv |
Cuaternario |
dc.publisher.es_PE.fl_str_mv |
The Geochemical Society of Japan |
dc.publisher.country.es_PE.fl_str_mv |
JP |
dc.source.es_PE.fl_str_mv |
Repositorio Institucional INGEMMET Instituto Geológico, Minero y Metalúrgico – INGEMMET |
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Kaneoka, IchiroGuevara Rosillo, CarlosAndesArequipaPunoPerúCuaternario2018-06-22T21:26:53Z2018-06-22T21:26:53Z1984Kaneoka, I. & Guevara, C. (1984) - K-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peru. Geochemical Journal, 18(5): 233–239. Doi: 10.2343/geochemj.18.233https://hdl.handle.net/20.500.12544/1505https://doi.org/10.2343/geochemj.18.233Geochemical JournalGeochemical Journal, 18(5): 233–239, 1984K-Ar ages were determined on 30 Andean volcanic rocks from southern Peru, most of which were considered to belong to the Barroso Group of Quaternary in age. The results have revealed, however, that their ages range from late Miocene to recent (7.2 to less than 0.03 Ma). This indicates that the Barroso Group samples might include much wider age ranges than had been assigned. Relatively young volcanic activity of late Quaternary is apparently restricted in the northwestern part including the vicinity of Arequipa in the investigated area. The main volcanic activity in the southwestern part seem to have almost ended by early Pleistocene. The shoshonitic rocks which are located around the Puno area probably extruded about 6Ma ago in a relatively short period of less than a few hundred thousand years.Peer reviewedapplication/pdfengThe Geochemical Society of JapanJPurn:issn:1880-5973info:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-sa/4.0/Repositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETDatación K-ArGeocronologíaRocas volcánicasGrupo SenccaGrupo TacazaK-Ar age determinations of the late Tertiary and Quaternary Andean volcanic rocks, southern Peruinfo:eu-repo/semantics/articleGeologíaORIGINAL1984-Kaneoka-K-Ar_age_determinations.pdf1984-Kaneoka-K-Ar_age_determinations.pdfArtículoapplication/pdf2009428https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1505/1/1984-Kaneoka-K-Ar_age_determinations.pdff47ceb62ff899a6f768bc2403f571a02MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1505/2/license.txtecccc10c448afdeacc04912e07a3ed65MD52THUMBNAIL1984-Kaneoka-K-Ar_age_determinations.pdf.jpg1984-Kaneoka-K-Ar_age_determinations.pdf.jpgGenerated Thumbnailimage/jpeg27770https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1505/4/1984-Kaneoka-K-Ar_age_determinations.pdf.jpg7e4b99243c37ad3c7a6343ca6fa131d3MD54TEXT1984-Kaneoka-K-Ar_age_determinations.pdf.txt1984-Kaneoka-K-Ar_age_determinations.pdf.txtExtracted texttext/plain23117https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/1505/3/1984-Kaneoka-K-Ar_age_determinations.pdf.txt05ce8914c9a3db87adeb55ddafb38b76MD5320.500.12544/1505oai:repositorio.ingemmet.gob.pe:20.500.12544/15052019-05-06 11:30:39.098Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.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 |
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La información contenida en este registro es de entera responsabilidad de la institución que gestiona el repositorio institucional donde esta contenido este documento o set de datos. El CONCYTEC no se hace responsable por los contenidos (publicaciones y/o datos) accesibles a través del Repositorio Nacional Digital de Ciencia, Tecnología e Innovación de Acceso Abierto (ALICIA).