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.contributorWeber, Marion
dc.contributorGómez-Tuena, Arturo
dc.creatorErrazuriz Henao, Carlos
dc.date.accessioned2021-08-30T21:44:35Z
dc.date.accessioned2022-09-21T17:50:20Z
dc.date.available2021-08-30T21:44:35Z
dc.date.available2022-09-21T17:50:20Z
dc.date.created2021-08-30T21:44:35Z
dc.date.issued2019
dc.identifierhttps://repositorio.unal.edu.co/handle/unal/80055
dc.identifierUniversidad Nacional de Colombia
dc.identifierRepositorio Institucional Universidad Nacional de Colombia
dc.identifierhttps://repositorio.unal.edu.co/
dc.identifier.urihttp://repositorioslatinoamericanos.uchile.cl/handle/2250/3403889
dc.description.abstractLa 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)
dc.description.abstractThe 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.
dc.languagespa
dc.publisherUniversidad Nacional de Colombia - Sede Medellín
dc.publisherMedellín - Minas - Maestría en Ingeniería - Recursos Minerales
dc.publisherDepartamento de Geociencias y Medo Ambiente
dc.publisherFacultad de Minas
dc.publisherMedellín
dc.publisherUniversidad Nacional de Colombia - Sede Medellín
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dc.rightsAtribución-SinDerivadas 4.0 Internacional
dc.rightshttp://creativecommons.org/licenses/by-nd/4.0/
dc.rightsinfo:eu-repo/semantics/openAccess
dc.titlePetrogénesis 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.typeTesis


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