Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships

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In the Central Andes of Peru, four volcanic arcs, termed Tacaza, Lower and Upper Barroso, and Frontal arc, have been active over the past 30 Ma (Fig. 1). They form five units between Moquegua and Nazca (14°30– 17°15’°S and 70–74°W). The ‘Neogene ignimbrites’ (<25 Ma) comprise six generations of w...

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Detalles Bibliográficos
Autores: Thouret, Jean-Claude, Mamani Huisa, Mirian Irene, Wörner, Gerhard, Paquereau-Lebti, Perrine, Gerbe, Marie Christine, Delacour, Adélie, Rivera Porras, Marco Antonio, Cacya Dueñas, Lourdes, Mariño Salazar, Jersy, Singer, Bradley S.
Formato: objeto de conferencia
Fecha de Publicación:2008
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:inglés
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/3803
Enlace del recurso:https://hdl.handle.net/20.500.12544/3803
Nivel de acceso:acceso abierto
Materia:Volcanes
Ignimbritas
Estratigrafía
Tefrocronología
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 Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
title Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
spellingShingle Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
Thouret, Jean-Claude
Volcanes
Ignimbritas
Estratigrafía
Tefrocronología
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
title_short Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
title_full Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
title_fullStr Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
title_full_unstemmed Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
title_sort Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships
author Thouret, Jean-Claude
author_facet Thouret, Jean-Claude
Mamani Huisa, Mirian Irene
Wörner, Gerhard
Paquereau-Lebti, Perrine
Gerbe, Marie Christine
Delacour, Adélie
Rivera Porras, Marco Antonio
Cacya Dueñas, Lourdes
Mariño Salazar, Jersy
Singer, Bradley S.
author_role author
author2 Mamani Huisa, Mirian Irene
Wörner, Gerhard
Paquereau-Lebti, Perrine
Gerbe, Marie Christine
Delacour, Adélie
Rivera Porras, Marco Antonio
Cacya Dueñas, Lourdes
Mariño Salazar, Jersy
Singer, Bradley S.
author2_role author
author
author
author
author
author
author
author
author
dc.contributor.author.fl_str_mv Thouret, Jean-Claude
Mamani Huisa, Mirian Irene
Wörner, Gerhard
Paquereau-Lebti, Perrine
Gerbe, Marie Christine
Delacour, Adélie
Rivera Porras, Marco Antonio
Cacya Dueñas, Lourdes
Mariño Salazar, Jersy
Singer, Bradley S.
dc.subject.es_PE.fl_str_mv Volcanes
Ignimbritas
Estratigrafía
Tefrocronología
topic Volcanes
Ignimbritas
Estratigrafía
Tefrocronología
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 In the Central Andes of Peru, four volcanic arcs, termed Tacaza, Lower and Upper Barroso, and Frontal arc, have been active over the past 30 Ma (Fig. 1). They form five units between Moquegua and Nazca (14°30– 17°15’°S and 70–74°W). The ‘Neogene ignimbrites’ (<25 Ma) comprise six generations of widespread sheets (>500 km2 and >20 km3 each), representing a major crustal melting event, triggered by thickening and advective heat input from the mantle wedge. Also, four generations of edifices (i.e shields, composite cones, and dome clusters) and monogenetic fields mostly overly the ignimbrites based on ages, stratigraphy and mapping.
publishDate 2008
dc.date.accessioned.none.fl_str_mv 2022-04-22T16:32:56Z
dc.date.available.none.fl_str_mv 2022-04-22T16:32:56Z
dc.date.issued.fl_str_mv 2008
dc.type.es_PE.fl_str_mv info:eu-repo/semantics/conferenceObject
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dc.identifier.citation.es_PE.fl_str_mv Thouret, J.; Mamani, M.; Wörner, G.; Paquereau-Lebti, P.; Gerbe, M.; Delacour, A.; Rivera, M.; Cacya, L.; Mariño, J. & Singer, B. (2008). Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships. En: International Symposium on Andean Geodynamics, 7. Nice, 2008. Extended abstracts. Paris: IRD Éditions, p. 545-548.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/3803
dc.identifier.bibliographicCitation.es_PE.fl_str_mv 7th International Symposium on Andean Geodynamics (ISAG 2008, Nice), 2-4 September, 2008, Extended Abstracts.
identifier_str_mv Thouret, J.; Mamani, M.; Wörner, G.; Paquereau-Lebti, P.; Gerbe, M.; Delacour, A.; Rivera, M.; Cacya, L.; Mariño, J. & Singer, B. (2008). Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships. En: International Symposium on Andean Geodynamics, 7. Nice, 2008. Extended abstracts. Paris: IRD Éditions, p. 545-548.
7th International Symposium on Andean Geodynamics (ISAG 2008, Nice), 2-4 September, 2008, Extended Abstracts.
url https://hdl.handle.net/20.500.12544/3803
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 Cotahuasi
Arequipa
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 Thouret, Jean-ClaudeMamani Huisa, Mirian IreneWörner, GerhardPaquereau-Lebti, PerrineGerbe, Marie ChristineDelacour, AdélieRivera Porras, Marco AntonioCacya Dueñas, LourdesMariño Salazar, JersySinger, Bradley S.CotahuasiArequipaPerú2022-04-22T16:32:56Z2022-04-22T16:32:56Z2008Thouret, J.; Mamani, M.; Wörner, G.; Paquereau-Lebti, P.; Gerbe, M.; Delacour, A.; Rivera, M.; Cacya, L.; Mariño, J. & Singer, B. (2008). Neogene ignimbrites and volcanic edifices in southern Peru: Stratigraphy and time-volume-composition relationships. En: International Symposium on Andean Geodynamics, 7. Nice, 2008. Extended abstracts. Paris: IRD Éditions, p. 545-548.https://hdl.handle.net/20.500.12544/38037th International Symposium on Andean Geodynamics (ISAG 2008, Nice), 2-4 September, 2008, Extended Abstracts.In the Central Andes of Peru, four volcanic arcs, termed Tacaza, Lower and Upper Barroso, and Frontal arc, have been active over the past 30 Ma (Fig. 1). They form five units between Moquegua and Nazca (14°30– 17°15’°S and 70–74°W). The ‘Neogene ignimbrites’ (<25 Ma) comprise six generations of widespread sheets (>500 km2 and >20 km3 each), representing a major crustal melting event, triggered by thickening and advective heat input from the mantle wedge. 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