Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons

Descripción del Articulo

3 páginas
Detalles Bibliográficos
Autores: Bahlburg, Heinrich, Vervoort, Jeffrey D., Du Frane, S. Andrew, Carlotto Caillaux, Víctor Santiago
Formato: objeto de conferencia
Fecha de Publicación:2008
Institución:Instituto Geológico, Minero y Metalúrgico
Repositorio:INGEMMET-Institucional
Lenguaje:español
OAI Identifier:oai:repositorio.ingemmet.gob.pe:20.500.12544/3430
Enlace del recurso:https://hdl.handle.net/20.500.12544/3430
Nivel de acceso:acceso abierto
Materia:Volcanismo
Datación U-Pb
Geocronología
Isótopos de hafnio
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
Formación Ollantaytambo
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dc.title.es_PE.fl_str_mv Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
title Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
spellingShingle Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
Bahlburg, Heinrich
Volcanismo
Datación U-Pb
Geocronología
Isótopos de hafnio
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
Formación Ollantaytambo
title_short Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
title_full Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
title_fullStr Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
title_full_unstemmed Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
title_sort Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
author Bahlburg, Heinrich
author_facet Bahlburg, Heinrich
Vervoort, Jeffrey D.
Du Frane, S. Andrew
Carlotto Caillaux, Víctor Santiago
author_role author
author2 Vervoort, Jeffrey D.
Du Frane, S. Andrew
Carlotto Caillaux, Víctor Santiago
author2_role author
author
author
dc.contributor.author.fl_str_mv Bahlburg, Heinrich
Vervoort, Jeffrey D.
Du Frane, S. Andrew
Carlotto Caillaux, Víctor Santiago
dc.subject.es_PE.fl_str_mv Volcanismo
Datación U-Pb
Geocronología
Isótopos de hafnio
topic Volcanismo
Datación U-Pb
Geocronología
Isótopos de hafnio
http://purl.org/pe-repo/ocde/ford#1.05.00
http://purl.org/pe-repo/ocde/ford#1.05.06
Formación Ollantaytambo
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
dc.subject.geology.es_PE.fl_str_mv Formación Ollantaytambo
description 3 páginas
publishDate 2008
dc.date.accessioned.none.fl_str_mv 2021-11-09T22:12:03Z
dc.date.available.none.fl_str_mv 2021-11-09T22:12:03Z
dc.date.issued.fl_str_mv 2008
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status_str publishedVersion
dc.identifier.citation.es_PE.fl_str_mv Rivera, M.; Vervoort, J.; Du Frane, S. & Carlotto, V. (2008) - Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons. En: Congreso Peruano de Geología, 14, Lima, 2008. Resúmenes. Lima: Sociedad Geológica del Perú, 3 p.
dc.identifier.uri.none.fl_str_mv https://hdl.handle.net/20.500.12544/3430
dc.identifier.bibliographicCitation.es_PE.fl_str_mv XIV Congreso Peruano de Geología, Lima, 29 setiembre - 3 octubre 2008. Resúmenes.
identifier_str_mv Rivera, M.; Vervoort, J.; Du Frane, S. & Carlotto, V. (2008) - Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons. En: Congreso Peruano de Geología, 14, Lima, 2008. Resúmenes. Lima: Sociedad Geológica del Perú, 3 p.
XIV Congreso Peruano de Geología, Lima, 29 setiembre - 3 octubre 2008. Resúmenes.
url https://hdl.handle.net/20.500.12544/3430
dc.language.iso.es_PE.fl_str_mv spa
language spa
dc.rights.es_PE.fl_str_mv info:eu-repo/semantics/openAccess
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dc.format.es_PE.fl_str_mv application/pdf
dc.coverage.spatial.es_PE.fl_str_mv Cusco
Perú
dc.publisher.es_PE.fl_str_mv Sociedad Geológica del Perú
dc.publisher.country.es_PE.fl_str_mv PE
dc.source.es_PE.fl_str_mv Repositorio Institucional INGEMMET
Instituto Geológico, Minero y Metalúrgico – INGEMMET
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instname:Instituto Geológico, Minero y Metalúrgico
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spelling Bahlburg, HeinrichVervoort, Jeffrey D.Du Frane, S. AndrewCarlotto Caillaux, Víctor SantiagoCuscoPerú2021-11-09T22:12:03Z2021-11-09T22:12:03Z2008Rivera, M.; Vervoort, J.; Du Frane, S. & Carlotto, V. (2008) - Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons. En: Congreso Peruano de Geología, 14, Lima, 2008. Resúmenes. Lima: Sociedad Geológica del Perú, 3 p.https://hdl.handle.net/20.500.12544/3430XIV Congreso Peruano de Geología, Lima, 29 setiembre - 3 octubre 2008. Resúmenes.3 páginasThe plate-tectonic setting of the Ordovician sedimcntary basin of southem Peru and northem Bolivia has been diversely intcrpreted as that of an intracmtonic marginal basin, an aulaoogen, a backarc rift or a passive margin (see summary in Bahlburg et al., 2006). The basin developed on a crustal collage represented by the Arequipa Massif as part of the Arequipa Terrane to the west and the Amazonia craton to the east (Fig. 1). The Arequipa Massif in tum, is part of a 1.9 to 1.8 Ga are terrane (Loewy and Bahlburg, 2007), which is considered to have docked against the SW Amazonia craton in Grenvillian time leading to the formation of the Sunsás orogenic belt in southwestem Brazil and eastem Bolivia (Fig. 1; Lithedand et al., 1989; Loewy et al., 2004). Geochronologic data demonstrated that early Paleozoic granitoids intruded into the Arequipa Massif have an Ordovician age (473-440 Ma, Womer' et al., 2000; Loewy et al., 2004). Early results of an ongoing geochemical study characterize these rocks as having formed in a magmatic are environment (Loewy and Bablburg, unpublished data). The only evidence of early Paleozoic volcanism in the northcm central Andes of northem Bolivia and southern Pero is represented by the mafic to intermediate lapilli tuffs of the Ordovician Ollantaytambo Formation and Umachiri beds in the Cordillera Oriental and Altiplano of southern Peru (Bahlburg et al., 2006).application/pdfspaSociedad Geológica del PerúPEinfo:eu-repo/semantics/openAccesshttps://creativecommons.org/licenses/by-nc-sa/4.0/deed.esRepositorio Institucional INGEMMETInstituto Geológico, Minero y Metalúrgico – INGEMMETreponame:INGEMMET-Institucionalinstname:Instituto Geológico, Minero y Metalúrgicoinstacron:INGEMMETVolcanismoDatación U-PbGeocronologíaIsótopos de hafniohttp://purl.org/pe-repo/ocde/ford#1.05.00http://purl.org/pe-repo/ocde/ford#1.05.06Formación OllantaytamboProvenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zirconsinfo:eu-repo/semantics/conferenceObjectinfo:eu-repo/semantics/publishedVersionORIGINALBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdfBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdfArticulo de congresoapplication/pdf1148023https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/1/Bahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf09d5bc9e8ff787e5046341b96b8eb55aMD51LICENSElicense.txtlicense.txttext/plain; charset=utf-81567https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/3/license.txtecccc10c448afdeacc04912e07a3ed65MD53TEXTBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.txtBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.txtExtracted texttext/plain3https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/4/Bahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.txt2228e977ebea8966e27929f43e39cb67MD54Bahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.txtBahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.txtExtracted texttext/plain7657https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/6/Bahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.txt4da6c0fee3897b99c3a4bc7c023c3ab0MD56THUMBNAILBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.jpgBahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.jpgGenerated Thumbnailimage/jpeg20447https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/5/Bahlburg-Provenance_early_paleozoic_Ollantaytambo.pdf.jpg66cdf5afbb4770660797df24e00b576aMD55Bahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.jpgBahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.jpgGenerated Thumbnailimage/jpeg23851https://repositorio.ingemmet.gob.pe/bitstream/20.500.12544/3430/7/Bahlburg-Provenance_early_paleozoic_Ollantaytambo-ocr.pdf.jpg422e58834469ae9ba55db9085bbf5163MD5720.500.12544/3430oai:repositorio.ingemmet.gob.pe:20.500.12544/34302021-11-09 18:28:06.103Repositorio Institucional INGEMMETrepositorio@ingemmet.gob.peTGljZW5jaWEgZGUgVXNvCgpFbCBJbnN0aXR1dG8gR2VvbMOzZ2ljbywgTWluZXJvIHkgTWV0YWzDunJnaWNvIOKAkyBJTkdFTU1FVCwgZGlmdW5kZSBtZWRpYW50ZSBzdSByZXBvc2l0b3JpbyBsYSBwcm9kdWNjacOzbiBjaWVudMOtZmljYSB5IHTDqWNuaWNhIHByb2R1Y2lkYSBwb3IgbG9zIG1pZW1icm9zIGRlIGxhIGluc3RpdHVjacOzbi4gRWwgY29udGVuaWRvIGRlIGxvcyBkb2N1bWVudG9zIGRpZ2l0YWxlcyBlcyBkZSBhY2Nlc28gYWJpZXJ0byBwYXJhIHRvZGEgcGVyc29uYSBpbnRlcmVzYWRhLgoKU2UgYWNlcHRhIGxhIGRpZnVzacOzbiBww7pibGljYSBkZSBsYSBvYnJhLCBzdSBjb3BpYSB5IHJlcHJvZHVjacOzbi4gUGFyYSBlbGxvIGVzIG5lY2VzYXJpbyBxdWUgc2UgY3VtcGxhIGNvbiBsYXMgc2lndWllbnRlcyBjb25kaWNpb25lczoKLSBFbCBuZWNlc2FyaW8gcmVjb25vY2ltaWVudG8gZGUgbGEgYXV0b3LDrWEgZGUgbGEgb2JyYSwgaWRlbnRpZmljYW5kbyBvcG9ydHVuYSB5IGNvcnJlY3RhbWVudGUgYSBsYSBwZXJzb25hIHF1ZSBwb3NlYSBsb3MgZGVyZWNob3MgZGUgYXV0b3IuCi0gTm8gZXN0w6EgcGVybWl0aWRvIGVsIHVzbyBpbmRlYmlkbyBkZSBsYSBvYnJhIGNvbiBmaW5lcyBkZSBsdWNybyBvIGN1YWxxdWllciB0aXBvIGRlIGFjdGl2aWRhZCBxdWUgcHJvZHV6Y2EgZ2FuYW5jaWFzIGEgbGFzIHBlcnNvbmFzIHF1ZSBsbyBkaWZ1bmRlbiBzaW4gZWwgY29uc2VudGltaWVudG8gZGVsIGF1dG9yLgotIExvcyB0cmFiYWpvcyBxdWUgc2UgcHJvZHV6Y2FuIGEgcGFydGlyIGRlIGxhIG9icmEgZGViZW4gcG9zZWVyIGxhIGNpdGFjacOzbiBwZXJ0aW5lbnRlIGRlIGFjdWVyZG8gYSBjdWFscXVpZXJhIGRlIGxvcyBlc3RpbG9zIChBUEEsIElTTywgVmFuY3V2ZXIsIGV0YykgZWxlZ2lkb3MgcGFyYSBsYSByZWRhY2Npw7NuIGRlIGxhcyByZWZlcmVuY2lhcyBiaWJsaW9ncsOhZmljYXMuIENhc28gY29udHJhcmlvIHNlIGluY3Vycmlyw6EgZW4gbGEgZmlndXJhIGp1csOtZGljYSBkZWwgcGxhZ2lvLgoKTG9zIGRlcmVjaG9zIG1vcmFsZXMgZGVsIGF1dG9yIG5vIHNvbiBhZmVjdGFkb3MgcG9yIGxhIHByZXNlbnRlIGxpY2VuY2lhIGRlIHVzby4KCkRlcmVjaG9zIGRlIGF1dG9yCgpMb3MgZGVyZWNob3MgZGUgYXV0b3Igc2UgZW5jdWVudHJhbiBwcm90ZWdpZG9zIHBvciBsYSBsZWdpc2xhY2nDs24gcGVydWFuYTogTGV5IHNvYnJlIGVsIERlcmVjaG8gZGUgQXV0b3IgcHJvbXVsZ2FkbyBlbiAxOTk2IChELkwuIE7CsCA4MjIpLCBMZXkgcXVlIG1vZGlmaWNhIGxvcyBhcnTDrWN1bG9zIDE4OMKweSAxODnCsCBkZWwgZGVjcmV0byBsZWdpc2xhdGl2byBOwrAgODIyLCBMZXkgc29icmUgRGVyZWNob3MgZGUgQXV0b3IgcHJvbXVsZ2FkYSBlbiAyMDA1IChMZXkgTsKwIDI4NTE3KSwgRGVjcmV0byBMZWdpc2xhdGl2byBxdWUgYXBydWViYSBsYSBtb2RpZmljYWNpw7NuIGRlbCBEZWNyZXRvIExlZ2lzbGF0aXZvIE7CsCA4MjIsIExleSBzb2JyZSBlbCBEZXJlY2hvIGRlIEF1dG9yIHByb211bGdhZG8gZW4gMjAwOCAoRC5MLiBOwrAgMTA3NikuCg==
score 13.887739
Provenance of the early Paleozoic Ollantaytambo Formation, southern Peru: the U-Pb and Hf isotope evidence of detrital zircons
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