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...

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Detalles Bibliográficos
Autores: Kaneoka, Ichiro, Guevara Rosillo, Carlos
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
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eu_rights_str_mv openAccess
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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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spelling 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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