Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization

Ilustraciones, mapas

Autores:: Botello Díaz, Gladys Eliana

Tipo de recurso:

Fecha de publicación:: 2024

Institución:: Universidad Nacional de Colombia

Repositorio:: Universidad Nacional de Colombia

Idioma:: eng

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network_acronym_str	UNACIONAL2
network_name_str	Universidad Nacional de Colombia
repository_id_str
dc.title.eng.fl_str_mv	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
dc.title.translated.spa.fl_str_mv	Petrogénesis del plutonismo Mioceno Inferior expuesto en la Cordillera Occidental de Colombia, y su relación con la reorganización de la subducción Neógena
title	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
spellingShingle	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization 550 - Ciencias de la tierra::552 - Petrología 550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur Petrogénesis - Colombia Estatigrafía - Mioceno - Colombia Magmatismo - América Geoquímica - Colombia Lower Miocene magmatism Neogene subduction geochemistry Zircon Hf isotopy mineral chemistry Magmatismo Mioceno Inferior Subducción Neógena Geoquímica Isotopía Lu-Hf en circón Química mineral
title_short	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
title_full	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
title_fullStr	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
title_full_unstemmed	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
title_sort	Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization
dc.creator.fl_str_mv	Botello Díaz, Gladys Eliana
dc.contributor.advisor.none.fl_str_mv	Siachoque Velandia, Astrid Cardona Molina, Agustin
dc.contributor.author.none.fl_str_mv	Botello Díaz, Gladys Eliana
dc.contributor.researchgroup.spa.fl_str_mv	Grupo de Estudios en Geología y Geofísica Egeo
dc.contributor.orcid.spa.fl_str_mv	0000-0001-5896-8709
dc.contributor.cvlac.spa.fl_str_mv	Botello Díaz, Gladys Eliana
dc.subject.ddc.spa.fl_str_mv	550 - Ciencias de la tierra::552 - Petrología 550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur
topic	550 - Ciencias de la tierra::552 - Petrología 550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur Petrogénesis - Colombia Estatigrafía - Mioceno - Colombia Magmatismo - América Geoquímica - Colombia Lower Miocene magmatism Neogene subduction geochemistry Zircon Hf isotopy mineral chemistry Magmatismo Mioceno Inferior Subducción Neógena Geoquímica Isotopía Lu-Hf en circón Química mineral
dc.subject.lemb.none.fl_str_mv	Petrogénesis - Colombia Estatigrafía - Mioceno - Colombia Magmatismo - América Geoquímica - Colombia
dc.subject.proposal.eng.fl_str_mv	Lower Miocene magmatism Neogene subduction geochemistry Zircon Hf isotopy mineral chemistry
dc.subject.proposal.spa.fl_str_mv	Magmatismo Mioceno Inferior Subducción Neógena Geoquímica Isotopía Lu-Hf en circón Química mineral
description	Ilustraciones, mapas
publishDate	2024
dc.date.accessioned.none.fl_str_mv	2024-07-11T17:16:47Z
dc.date.available.none.fl_str_mv	2024-07-11T17:16:47Z
dc.date.issued.none.fl_str_mv	2024
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/86430
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/86430 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	eng
language	eng
dc.relation.indexed.spa.fl_str_mv	LaReferencia
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dc.format.extent.spa.fl_str_mv	105 páginas
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dc.publisher.spa.fl_str_mv	Universidad Nacional de Colombia sede Medellín
dc.publisher.program.spa.fl_str_mv	Medellín - Minas - Maestría en Ingeniería - Recursos Minerales
dc.publisher.faculty.spa.fl_str_mv	Facultad de Minas
dc.publisher.place.spa.fl_str_mv	Medellín, Colombia
dc.publisher.branch.spa.fl_str_mv	Universidad Nacional de Colombia - Sede Medellín
institution	Universidad Nacional de Colombia
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spelling	Atribución-NoComercial-SinDerivadas 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-nd/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Siachoque Velandia, Astrid0e2b11dc0c5bd9f51e26f516332f53f5Cardona Molina, Agustin2fa1e9f10a30d8eaa598c672ee859588Botello Díaz, Gladys Eliana1b248f26830527506e0d54720d8255e0Grupo de Estudios en Geología y Geofísica Egeo0000-0001-5896-8709Botello Díaz, Gladys Eliana2024-07-11T17:16:47Z2024-07-11T17:16:47Z2024https://repositorio.unal.edu.co/handle/unal/86430Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/Ilustraciones, mapasLower Miocene plutons exposed in the Western Cordillera of Colombia record the reinitiation of continental arc magmatism in the Northern Andes after a period of magmatic quiescence between the Late Eocene and Early Miocene. Petrography, U-Pb zircon geochronology, whole-rock geochemistry, mineral chemistry, and zircon Hf isotope data from these plutons are used to reconstruct the Miocene magmatic evolution in the Colombian Andes and understand its relation with the major plate-tectonic reorganization experienced by the NW South American continental margin during the Lower Miocene. We examined a suite of gabbros, granodiorites and tonalites from Danubio, Pance and Tatamá plutons, formed between 21 Ma and 15 Ma. Gabbros present highly positive εHf values (+13.5 and +11.5) with low Th/La and La/Yb ratios, whereas granodiorites and tonalites present lower εHf values (+14.3 to +6.4) and high Th/La, and La/Yb ratios. The results of this contribution suggest a major asthenospheric source metasomatized by oxidized aqueous fluids derived from the subducted components. The compositional diversification of these magmas was controlled by fractional crystallization and possibly by minor assimilation of continental crust at lower crustal levels of the upper plate and by magma mixing processes. Subsequently, these magmas were emplaced in the Cretaceous to Paleogene volcanic and sedimentary rocks in the uppermost crust. The renewed magmatic activity recorded by these plutons can be related to the early stages of the Neogene plate reorganization, which was characterized by the normal to steep subduction of the Farallon Plate remnants. (Tomado de la fuente)Los plutones del Mioceno inferior expuestos en la Cordillera Occidental de Colombia registran el reinicio del magmatismo del arco continental en los Andes del Norte después de un período de inactividad magmática entre el Eoceno Tardío y el Mioceno Temprano. La petrografía, la geocronología U-Pb en circón, la geoquímica de roca total, la química mineral y los datos de isótopos de Hf en circón de estos plutones se utilizan para reconstruir la evolución magmática del Mioceno en los Andes colombianos y comprender su relación con la reorganización de placas tectónicas experimentada por el margen continental noroeste de América del Sur durante el Mioceno Inferior. Examinamos un conjunto de gabros, granodioritas y tonalitas de los plutones El Danubio, Pance y Tatamá, formados entre 21 Ma y 15 Ma. Los gabros presentan valores de εHf muy positivos (+13,5 y +11,5) con relaciones Th/La y La/Yb bajas, mientras que las granodioritas y tonalitas presentan valores de εHf más bajos (+14,3 a +6,4) y relaciones Th/La y La/Yb altas. Los resultados de este trabajo sugieren una fuente astenosférica metasomatizada por fluidos acuosos oxidados derivados de los componentes subducidos. La diversificación composicional de estos magmas estuvo controlada por procesos de cristalización fraccionada, así como posiblemente por una asimilación limitada de corteza continental en el nivel inferior de la placa superior y por procesos de mezcla de magma. Posteriormente, estos magmas se emplazaron en rocas volcánicas y sedimentarias del Cretácico al Paleógeno presentes en niveles superiores de la corteza. La renovada actividad magmática registrada por estos plutones puede estar relacionada con las primeras etapas de la reorganización de la placa Neógena, que se caracterizó por la subducción normal a pronunciada de los remanentes de la Placa Farallón.MaestríaMaestría en Ingeniería - Recursos MineralesRecursos Minerales.Sede Medellín105 páginasapplication/pdfengUniversidad Nacional de Colombia sede MedellínMedellín - Minas - Maestría en Ingeniería - Recursos MineralesFacultad de MinasMedellín, ColombiaUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra::552 - Petrología550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del SurPetrogénesis - ColombiaEstatigrafía - Mioceno - ColombiaMagmatismo - AméricaGeoquímica - ColombiaLower Miocene magmatismNeogene subductiongeochemistryZircon Hf isotopymineral chemistryMagmatismo Mioceno InferiorSubducción NeógenaGeoquímicaIsotopía Lu-Hf en circónQuímica mineralPetrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organizationPetrogénesis del plutonismo Mioceno Inferior expuesto en la Cordillera Occidental de Colombia, y su relación con la reorganización de la subducción NeógenaTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMLaReferenciaAlexander, E., & Harrison, M. 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Servicio Geológico Colombiano, Publicaciones Geológicas Especiales 36, 171–207. https://doi.org/10.32685/pub.esp.36.2019.05Bayona, G., Cardona, A., Jaramillo, C., Mora, A., Montes, C., Valencia, V., Ayala, C., Montenegro, O., & Ibañez-Mejia, M. (2012). Early Paleogene magmatism in the northern Andes: Insights on the effects of Oceanic Plateau–continent convergence. Earth and Planetary Science Letters, 331–332, 97–111. https://doi.org/10.1016/j.epsl.2012.03.015Bell, E. A., & Kirkpatrick, H. M. (2021). Effects of crustal assimilation and magma mixing on zircon trace element relationships across the Peninsular Ranges Batholith. Chemical Geology, 586(120616), 120616. https://doi.org/10.1016/j.chemgeo.2021.120616Bernet, M & Garver, J., (2005). Fission-track analysis of detrital zircon. Reviews in Mineralogy and Geochemistry, 58(1), 205–237. https://doi.org/10.2138/rmg.2005.58.8Bernet, M. (2009). A field-based estimate of the zircon fission-track closure temperature. 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Earth-Science Reviews, 107(3–4), 342–374. https://doi.org/10.1016/j.earscirev.2011.04.004Grupo de Estudios en Geología y GeofísicaLICENSElicense.txtlicense.txttext/plain; charset=utf-85879https://repositorio.unal.edu.co/bitstream/unal/86430/1/license.txteb34b1cf90b7e1103fc9dfd26be24b4aMD51ORIGINAL1017255225.2024.pdf1017255225.2024.pdfTesis de Maestría en Ingeniería - Recursos Mineralesapplication/pdf6388316https://repositorio.unal.edu.co/bitstream/unal/86430/2/1017255225.2024.pdff49b423e3fae580f063a21747efa31eaMD52THUMBNAIL1017255225.2024.pdf.jpg1017255225.2024.pdf.jpgGenerated Thumbnailimage/jpeg5255https://repositorio.unal.edu.co/bitstream/unal/86430/3/1017255225.2024.pdf.jpgb8a8b9559491bceb2e69ef26eed9f571MD53unal/86430oai:repositorio.unal.edu.co:unal/864302024-07-11 23:28:52.093Repositorio Institucional Universidad Nacional de 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Petrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organization

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