Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.

ilustraciones, mapas

Autores:: Errazuriz Henao, Carlos

Tipo de recurso:

Fecha de publicación:: 2019

Institución:: Universidad Nacional de Colombia

Repositorio:: Universidad Nacional de Colombia

Idioma:: spa

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network_acronym_str	UNACIONAL2
network_name_str	Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
dc.title.translated.eng.fl_str_mv	Petrogenesis of the north Volcanic Province of Colombia: Tectonic implications on the reworking of subduction components and their impact in arc magmatism.
title	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
spellingShingle	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco. 550 - Ciencias de la tierra Andesites Subduction Panama Basin Andesitas Subducción Cuenca de Panama
title_short	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
title_full	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
title_fullStr	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
title_full_unstemmed	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
title_sort	Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.
dc.creator.fl_str_mv	Errazuriz Henao, Carlos
dc.contributor.advisor.none.fl_str_mv	Weber, Marion Gómez-Tuena, Arturo
dc.contributor.author.none.fl_str_mv	Errazuriz Henao, Carlos
dc.subject.ddc.spa.fl_str_mv	550 - Ciencias de la tierra
topic	550 - Ciencias de la tierra Andesites Subduction Panama Basin Andesitas Subducción Cuenca de Panama
dc.subject.proposal.eng.fl_str_mv	Andesites Subduction Panama Basin
dc.subject.proposal.spa.fl_str_mv	Andesitas Subducción Cuenca de Panama
description	ilustraciones, mapas
publishDate	2019
dc.date.issued.none.fl_str_mv	2019
dc.date.accessioned.none.fl_str_mv	2021-08-30T21:44:35Z
dc.date.available.none.fl_str_mv	2021-08-30T21:44:35Z
dc.type.spa.fl_str_mv	Trabajo de grado - Maestría
dc.type.driver.spa.fl_str_mv	info:eu-repo/semantics/masterThesis
dc.type.version.spa.fl_str_mv	info:eu-repo/semantics/acceptedVersion
dc.type.content.spa.fl_str_mv	Text
dc.type.redcol.spa.fl_str_mv	http://purl.org/redcol/resource_type/TM
status_str	acceptedVersion
dc.identifier.uri.none.fl_str_mv	https://repositorio.unal.edu.co/handle/unal/80055
dc.identifier.instname.spa.fl_str_mv	Universidad Nacional de Colombia
dc.identifier.reponame.spa.fl_str_mv	Repositorio Institucional Universidad Nacional de Colombia
dc.identifier.repourl.spa.fl_str_mv	https://repositorio.unal.edu.co/
url	https://repositorio.unal.edu.co/handle/unal/80055 https://repositorio.unal.edu.co/
identifier_str_mv	Universidad Nacional de Colombia Repositorio Institucional Universidad Nacional de Colombia
dc.language.iso.spa.fl_str_mv	spa
language	spa
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dc.format.extent.spa.fl_str_mv	viii, 132 páginas
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dc.publisher.spa.fl_str_mv	Universidad Nacional de Colombia - Sede Medellín
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dc.publisher.faculty.spa.fl_str_mv	Facultad de Minas
dc.publisher.place.spa.fl_str_mv	Medellín
dc.publisher.branch.spa.fl_str_mv	Universidad Nacional de Colombia - Sede Medellín
institution	Universidad Nacional de Colombia
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spelling	Atribución-SinDerivadas 4.0 Internacionalhttp://creativecommons.org/licenses/by-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Weber, Marion85d89d530d2c9e57fba8e6b0d3144134600Gómez-Tuena, Arturo41022218433ae73dab9d277d5cc7cf41600Errazuriz Henao, Carlos050404db066fd273f7993488844984be6002021-08-30T21:44:35Z2021-08-30T21:44:35Z2019https://repositorio.unal.edu.co/handle/unal/80055Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, mapasLa Provincia Volcánica del Norte (PVN) de los Andes del Norte colombianos está constituida por una secuencia de ~65 km de estratovolcanes alineados de N-S producto de la subducción de la placa relativamente joven de Nazca bajo el margen del continente suramericano. La columna sedimentaria subducida a lo largo de la trinchera colombiana está constituida por una unidad inferior rica en carbonato, cubierta por una secuencia hemipelágica rica en arcillas. Los productos volcánicos típicos de la PVN son lavas calco-alcalinas andesítico-dacíticas con un alto #Mg (> 58) que intruyen un basamento paleozoico relativamente uniforme de 40-50 km de espesor. A pesar de la homogeneidad de los productos volcánicos en términos de los elementos mayores, las rocas volcánicas exhiben una clara variación a lo largo del arco en elementos traza y composiciones isotópicas: los volcanes en los bordes al norte y sur de la provincia (i.e. Cerro Bravo y Cerro Machín) muestran una relación alta de Nb/Ta y Ba/Th, una relación baja de Th(U)/La y composiciones isotópicas de Sr-Nd-Hf más enriquecidas que los volcanes del centro (i.e. Santa Isabel). Estas variaciones no pueden explicarse por la asimilación cortical, por variaciones en el grado de fusión del manto o por cambios en los parámetros térmicos de la corteza oceánica subducida, ya que la arquitectura cortical es relativamente similar y la profundidad de la placa subducente aumenta gradualmente hacia el sur. En cambio, modelados geoquímicos indican que los volcanes en los bordes de la PVN incorporan una mayor proporción de sedimento carbonatado, mientras que los productos volcánicos hacia el centro tienen una mayor influencia de los componentes sedimentarios hemipelágicos. Debido a que el cese de la actividad magmática en los bordes de la NVP parece estar controlado por una segmentación de la subducción, se propone que un estado termal más alto producido por la desgarre de la placa Nazca en profundidad permite que una mayor incorporación del sedimento carbonatado sea retrabajado en los volcanes de los extremos. En contraste, los volcanes en el centro de la PVN, que están más alejados del desgarre de la placa, están ubicados sobre un régimen termal más frío que impide la fusión de las litologías refractarias propias de los sedimentos altamente carbonatados. (Texto tomado de la fuente)The Northern Volcanic Province (NVP) of the Colombian Andes is constituted by a ~65 km long N-S alignment of arc stratovolcanoes produced by the subduction of the young Nazca plate beneath the South American margin. The subducted sedimentary column along the Colombian trench is made up of a lower carbonate-rich unit covered by a hemipelagic clay sequence. The typical volcanic products of the NVP are high Mg# (>58) calc-alkaline andesitic-dacitic lavas built upon a uniform 40-50 km thick Paleozoic basement. Despite their homogeneity in terms of the major elements, the volcanic rocks exhibit a clear along-arc variation in trace elements and isotopic compositions: volcanoes at the northern and southern edges of the volcanic province (i.e. Cerro Bravo and Cerro Machín) display higher Nb/Ta and Ba/Th, lower Th(U)/La and more enriched Sr-Nd-Hf isotopic compositions than the volcanoes at the center (i.e. Santa Isabel). These variations cannot be explained by crustal assimilation, variations in the extent of mantle melting or changes in the slab thermal parameters because the crustal architecture is the same along strike and the slab depth gradually increases to the south. Instead, geochemical modelling indicates that volcanoes at the edges of the PVN incorporate a larger proportion of subducted sedimentary carbonate, while the volcanic products at the center have a greater influence of hemipelagic sediment components. Because the cessation of magmatic activity at the edges of the NVP appears to be controlled by a segmentation in the subducted slab, we propose that a higher thermal state produced by the slab-tear at depth allows a larger proportion of carbonate to be incorporated into the mantle source of the edge volcanoes. In contrast, volcanoes at the center of the chain, which are farther away from the slab-tear, are built upon a cooler thermal regime that hinders melting of the more refractory carbonate-rich lithologies.Colciencias - Proyecto Jóvenes InvestigadoresMaestríaMagíster en Ingeniería - Recursos MineralesPetrología ígnea y Geoquímicaviii, 132 páginasapplication/pdfspaUniversidad Nacional de Colombia - Sede MedellínMedellín - Minas - Maestría en Ingeniería - Recursos MineralesDepartamento de Geociencias y Medo AmbienteFacultad de MinasMedellínUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierraAndesitesSubductionPanama BasinAndesitasSubducciónCuenca de PanamaPetrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.Petrogenesis of the north Volcanic Province of Colombia: Tectonic implications on the reworking of subduction components and their impact in arc magmatism.Trabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMAiuppa, A., Fischer, T.P., Plank, T., Robidoux, P., Di Napoli, R., 2017. 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Gondwana Research. https://doi.org/10.1016/j.gr.2018.10.008EspecializadaLICENSElicense.txtlicense.txttext/plain; charset=utf-83964https://repositorio.unal.edu.co/bitstream/unal/80055/4/license.txtcccfe52f796b7c63423298c2d3365fc6MD54CC-LICENSElicense_rdflicense_rdfapplication/rdf+xml; charset=utf-8799https://repositorio.unal.edu.co/bitstream/unal/80055/6/license_rdff7d494f61e544413a13e6ba1da2089cdMD56ORIGINAL1152202988.2019.pdf1152202988.2019.pdfTesis de Maestría en Ingeniería - Recursos Mineralesapplication/pdf8288570https://repositorio.unal.edu.co/bitstream/unal/80055/7/1152202988.2019.pdfc5fcf29e64b5cc346dda33a695f514adMD57THUMBNAIL1152202988.2019.pdf.jpg1152202988.2019.pdf.jpgGenerated Thumbnailimage/jpeg5643https://repositorio.unal.edu.co/bitstream/unal/80055/8/1152202988.2019.pdf.jpg48851d8b22cd9b16d16e38e56fcb42c8MD58unal/80055oai:repositorio.unal.edu.co:unal/800552023-07-26 23:03:45.395Repositorio Institucional Universidad Nacional de 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GVyZWNob3MgZGUgYXV0b3IgcXVlIGNvbmxsZXZlIGxhIGRpc3RyaWJ1Y2nDs24gZGUgZXN0b3MgYXJjaGl2b3MgeSBtZXRhZGF0b3MuCkFsIGhhY2VyIGNsaWMgZW4gZWwgc2lndWllbnRlIGJvdMOzbiwgdXN0ZWQgaW5kaWNhIHF1ZSBlc3TDoSBkZSBhY3VlcmRvIGNvbiBlc3RvcyB0w6lybWlub3MuCgpVTklWRVJTSURBRCBOQUNJT05BTCBERSBDT0xPTUJJQSAtIMOabHRpbWEgbW9kaWZpY2FjacOzbiAyNy8yMC8yMDIwCg==

Petrogénesis de la Provincia Volcánica norte de Colombia: Implicaciones tectónicas en el retrabajamiento de los componentes en subducción y su impacto en el magmatismo de arco.

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