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

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dc.contributor.advisorSiachoque Velandia, Astrid
dc.contributor.advisorCardona Molina, Agustin
dc.contributor.authorBotello Díaz, Gladys Eliana
dc.contributor.cvlacBotello Díaz, Gladys Elianaspa
dc.contributor.orcid0000-0001-5896-8709spa
dc.contributor.researchgroupGrupo de Estudios en Geología y Geofísica Egeospa
dc.date.accessioned2024-07-11T17:16:47Z
dc.date.available2024-07-11T17:16:47Z
dc.date.issued2024
dc.descriptionIlustraciones, mapasspa
dc.description.abstractLower 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)eng
dc.description.abstractLos 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.spa
dc.description.curricularareaRecursos Minerales.Sede Medellínspa
dc.description.degreelevelMaestríaspa
dc.description.degreenameMaestría en Ingeniería - Recursos Mineralesspa
dc.format.extent105 páginasspa
dc.format.mimetypeapplication/pdfspa
dc.identifier.instnameUniversidad Nacional de Colombiaspa
dc.identifier.reponameRepositorio Institucional Universidad Nacional de Colombiaspa
dc.identifier.repourlhttps://repositorio.unal.edu.co/spa
dc.identifier.urihttps://repositorio.unal.edu.co/handle/unal/86430
dc.language.isoengspa
dc.publisherUniversidad Nacional de Colombia sede Medellínspa
dc.publisher.branchUniversidad Nacional de Colombia - Sede Medellínspa
dc.publisher.facultyFacultad de Minasspa
dc.publisher.placeMedellín, Colombiaspa
dc.publisher.programMedellín - Minas - Maestría en Ingeniería - Recursos Mineralesspa
dc.relation.indexedLaReferenciaspa
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dc.rights.accessrightsinfo:eu-repo/semantics/openAccessspa
dc.rights.licenseAtribución-NoComercial-SinDerivadas 4.0 Internacionalspa
dc.rights.urihttp://creativecommons.org/licenses/by-nc-nd/4.0/spa
dc.subject.ddc550 - Ciencias de la tierra::552 - Petrologíaspa
dc.subject.ddc550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Surspa
dc.subject.lembPetrogénesis - Colombia
dc.subject.lembEstatigrafía - Mioceno - Colombia
dc.subject.lembMagmatismo - América
dc.subject.lembGeoquímica - Colombia
dc.subject.proposalLower Miocene magmatismeng
dc.subject.proposalNeogene subductioneng
dc.subject.proposalgeochemistryeng
dc.subject.proposalZircon Hf isotopyeng
dc.subject.proposalmineral chemistryeng
dc.subject.proposalMagmatismo Mioceno Inferiorspa
dc.subject.proposalSubducción Neógenaspa
dc.subject.proposalGeoquímicaspa
dc.subject.proposalIsotopía Lu-Hf en circónspa
dc.subject.proposalQuímica mineralspa
dc.titlePetrogenesis of Early Miocene plutonism in the Western Cordillera of Colombia, and its relation with Neogene subduction re-organizationeng
dc.title.translatedPetrogénesis del plutonismo Mioceno Inferior expuesto en la Cordillera Occidental de Colombia, y su relación con la reorganización de la subducción Neógenaspa
dc.typeTrabajo de grado - Maestríaspa
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oaire.fundernameGrupo de Estudios en Geología y Geofísicaspa

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