Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes

Ilustraciones

Autores:: Jaramillo Ríos, Juan Sebastián

Tipo de recurso:: Doctoral thesis

Fecha de publicación:: 2024

Institución:: Universidad Nacional de Colombia

Repositorio:: Universidad Nacional de Colombia

Idioma:: eng

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repository_id_str
dc.title.eng.fl_str_mv	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
dc.title.translated.spa.fl_str_mv	Magmatismo como un trazador de la evolución cortical cenozoica de los Andes del Norte
title	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
spellingShingle	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología Magnetismo Isotopos Cronología geológica Geoquímica Magmatism U-Pb and Ar-Ar Geochronology Geochemistry Isotopes Dripping, Northern Andes Magmatismo Geocronología U-Pb y Ar-Ar Geoquímica Isotopos
title_short	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
title_full	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
title_fullStr	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
title_full_unstemmed	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
title_sort	Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes
dc.creator.fl_str_mv	Jaramillo Ríos, Juan Sebastián
dc.contributor.advisor.none.fl_str_mv	Cardona Molina, Agustín Zapata Henao, Sebastián
dc.contributor.author.none.fl_str_mv	Jaramillo Ríos, Juan Sebastián
dc.contributor.researchgroup.spa.fl_str_mv	Grupo de Estudios en Geología y Geofísica Egeo
dc.contributor.orcid.spa.fl_str_mv	https://orcid.org/0000-0003-1067-9259
dc.contributor.cvlac.spa.fl_str_mv	https://scienti.minciencias.gov.co/cvlac/visualizador/generarCurriculoCv.do?cod_rh=0001553908
dc.contributor.researchgate.spa.fl_str_mv	https://www.researchgate.net/profile/Juan-Jaramillo-Rios
dc.contributor.googlescholar.spa.fl_str_mv	https://scholar.google.com/citations?user=uMbRBRoAAAAJ&hl=es
dc.subject.ddc.spa.fl_str_mv	550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología
topic	550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología Magnetismo Isotopos Cronología geológica Geoquímica Magmatism U-Pb and Ar-Ar Geochronology Geochemistry Isotopes Dripping, Northern Andes Magmatismo Geocronología U-Pb y Ar-Ar Geoquímica Isotopos
dc.subject.lemb.none.fl_str_mv	Magnetismo Isotopos Cronología geológica Geoquímica
dc.subject.proposal.eng.fl_str_mv	Magmatism U-Pb and Ar-Ar Geochronology Geochemistry Isotopes Dripping, Northern Andes
dc.subject.proposal.spa.fl_str_mv	Magmatismo Geocronología U-Pb y Ar-Ar Geoquímica Isotopos
description	Ilustraciones
publishDate	2024
dc.date.accessioned.none.fl_str_mv	2024-07-08T18:40:32Z
dc.date.available.none.fl_str_mv	2024-07-08T18:40:32Z
dc.date.issued.none.fl_str_mv	2024-10-31
dc.type.spa.fl_str_mv	Trabajo de grado - Doctorado
dc.type.driver.spa.fl_str_mv	info:eu-repo/semantics/doctoralThesis
dc.type.version.spa.fl_str_mv	info:eu-repo/semantics/acceptedVersion
dc.type.coar.spa.fl_str_mv	http://purl.org/coar/resource_type/c_db06
dc.type.content.spa.fl_str_mv	Text
dc.type.redcol.spa.fl_str_mv	http://purl.org/redcol/resource_type/TD
format	http://purl.org/coar/resource_type/c_db06
status_str	acceptedVersion
dc.identifier.uri.none.fl_str_mv	https://repositorio.unal.edu.co/handle/unal/86412
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/86412 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
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Late Cretaceous to Paleocene magmatic record of the transition between collision and subduction in the Western and Central Cordillera of northern Colombia. Journal of South American Earth Sciences, 112, 103557. https://doi.org/10.1016/j.jsames.2021.103557 Zhao, L., Guo, F., Fan, W., & Huang, M. (2019). Roles of Subducted Pelagic and Terrigenous Sediments in Early Jurassic Mafic Magmatism in NE China: Constraints on the Architecture of Paleo-Pacific Subduction Zone. Journal of Geophysical Research: Solid Earth 124, 2525-2550. https://doi.org/10.1029/2018JB016487 Zieman, L., Ibañez-Mejia, M., Rooney, A. D., Bloch, E., Pardo, N., Schoene, B., & Szymanowski, D. (2023). To sink, or not to sink: The thermal and density structure of the modern northern Andean arc constrained by xenolith petrology. Geology, 51(6), 586-590. https://doi.org/10.1130/g50973.1 Zimmerer, M. J., & McIntosh, W. C. (2012). The geochronology of volcanic and plutonic rocks at the Questa caldera: Constraints on the origin of caldera-related silicic magmas. Bulletin of the Geological Society of America, 124(7-8), 1394-1408. https://doi.org/10.1130/B30544.1.
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dc.publisher.spa.fl_str_mv	Universidad Nacional de Colombia
dc.publisher.program.spa.fl_str_mv	Medellín - Minas - Doctorado en Ingeniería - Ciencia y Tecnología de Materiales
dc.publisher.faculty.spa.fl_str_mv	Facultad de Minas
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_abf2Cardona Molina, Agustín765d759de5d84bc9085321c1634df535Zapata Henao, Sebastián6e7ac60f6b7d382aa847138f38bc3acdJaramillo Ríos, Juan Sebastiánb0b9c69f6ee1a3c51c5d9e41b3c87e09Grupo de Estudios en Geología y Geofísica Egeohttps://orcid.org/0000-0003-1067-9259https://scienti.minciencias.gov.co/cvlac/visualizador/generarCurriculoCv.do?cod_rh=0001553908https://www.researchgate.net/profile/Juan-Jaramillo-Rioshttps://scholar.google.com/citations?user=uMbRBRoAAAAJ&hl=es2024-07-08T18:40:32Z2024-07-08T18:40:32Z2024-10-31https://repositorio.unal.edu.co/handle/unal/86412Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/IlustracionesIlustraciones, mapas a colorCrustal evolution in orogenic belts, such as the Northern Andes, has broadly been associated with subduction and mantle dynamics, the collision of allochthonous blocks, and the recycling of the lower crust into the asthenospheric mantle. All of these scenarios can produce magmatic rocks, which are sensitive enough to trace changes experienced by the continental crust. In this study, field relations, petrography, zircon U-Pb (LA-ICP-MS and CA-ID-TIMS) geochronology, geochemistry, and isotopes (Hf), as well as whole-rock geochemistry and isotopes (Nd-Sr-Pb) modeling, and 40Ar/39Ar geochronological data, were used to understand the magmatic evolution of the Paleocene-Eocene continental magmatic arc and the Pliocene-Pleistocene volcanic rocks recorded in the central segment of the modern Colombian magmatic arc. Therefore, these magmatic rocks were used as a tracer of the long-term modification of the continental crust in convergent margins. The Paleocene-Eocene (66 - 50 Ma) continental magmatic arc was formed after the collision of the Caribbean Plate with the Northern Andean continental margin at ~72 Ma. These rocks were highly exhumed and underwent high weathering and erosion rates, which resulted in the volcanic sources of this magmatism being transported to the sedimentary basins. In order to avoid sampling bias produced by the limited exposure of the plutonic facies of this magmatism, detrital zircons collected in sedimentary rocks were very important to understand the behavior of this magmatic arc. Siliciclastic rocks from the Bogotá Formation were analyzed by LA-ICP-MS and CA-ID-TIMS geochronology and zircon chemistry. The results show that this magmatism started at ~ 66 Ma, which is ~ 4 Myr earlier than previously proposed by other authors and ended at ~50 Ma. This magmatism was formed in a heterogeneously thick continental crust, strongly controlled by strike-slip tectonics. Finally, this study proposes lithospheric dripping into the mantle to explain the bi-modal continental crust thick between 62 and 55 Ma. After forming this arc, the continental margin was characterized by an oblique regime, which shut down the magmatic production between 50 and 35 Ma. The magmatic rocks restarted in the Western Cordillera as the Timbiquí arc and migrated toward the east up to where the modern magmatic arc is located. During the Pliocene-Pleistocene, the central segment of the modern Colombian magmatic arc is characterized by the production of contrasting magmatic rocks, including high-silica rhyolites, adakite-like andesites, and OIB-like alkaline basalts. The high-silica rhyolitic ignimbrites were formed during a high magmatic flux (magmatic flare-up) in this arc segment at 2.6 Ma. This study proposes that the high magma flux produces a significant volume of basaltic cumulates, which were ponded in the base of the crust, facilitating the formation of garnet-bearing pyroxenites known as arclogites. This magmatic flare-up could be related to an increased sediment input into the subducted slab, as suggested by the isotopic modeling. It is known that the arclogites in this arc segment are denser than the underlying mantle. It is proposed that Pleistocene olivine basalts and andesites associated with monogenetic volcanism found in this arc section are related to dripping rather than complete delamination of the lower crust into the asthenospheric mantle, originating from two distinct arclogites: one garnet-bearing and the other amphibole-garnet-bearing pyroxenite. The chapters developed in this thesis demonstrate how the continental margin of the Northernmost Andes has been dynamic throughout the Cenozoic era. Unlike the Central Andes, where orogeny is predominantly driven by subduction-dynamics shortening, the Colombian orogen is influenced by block collisions, strike-slip tectonics, and magmatic underplating. The magmatic underplating in this Andean section may have been the critical factor controlling the crustal thickness and subsequent removal of the lower, denser, and unstable portion of the lithosphere.La evolución de cinturones orogénicos como los Andes del Norte ha sido ampliamente asociado con la dinámica de la subducción y el mano, la colisión de bloques alóctonos y el reciclamiento de la corteza inferior dentro del manto astenosférico. Todos estos escenarios producen rocas magmáticas, las cuales son lo suficientemente sensibles para trazar los cambios experimentados por la corteza continental. En este estudio, relaciones de campo, petrografía, geocronología (LA-ICP-MS y CA-ID-TIMS), química e isotopía (Hf) en circón, así como modelamiento geoquímico e isotópico (Nd-Sr-Pb) en roca total, y geocronología Ar-Ar en masa fundamental, se usaron para entender la evolución magmática del arco Paleoceno-Eoceno y rocas volcánicas del Plioceno-Pleistoceno del orógeno Nor-Andino. Estas rocas, por lo tanto, fueron usadas como trazadoras de las modificaciones de la corteza continental en márgenes continentales. Posterior a la colusión de la Placa Caribe con la margen Nor-Andina a ~72 Ma, se formó un arco postcolisional del Paleoceno-Eoceno (66 – 50 Ma). Estas rocas junto con su basamento fueron rápidamente exhumadas y registran altas tasas de meteorización y erosión. Con el fin de evitar el sesgo de muestreo producido por la exposición limitada de las fases magmáticas proximales, circones detríticos fueron colectados en las rocas siliciclásticas de la Formación Bogotá. Estos circones fueron químicamente analizados y datados mediante geocronología LA-ICP-MS y CA-ID-TIMS. Los resultados muestras que este arco magmático comenzó a ~ 66 Ma, lo cual es ~ 4 Ma más temprano de lo que previamente se había propuesto por otros autores y termina a ~50 Ma. Este magmatismo se formó en una margen de espesor heterogéneo, fuertemente controlada por la tectónica de rumbo. Finalmente, este estudio propone que la litosfera fue removida “dripping” para explicar la bi-modalidad del espesor cortical entre 62 y 55 Ma. El segmento central del arco magmático reciente en Colombia durante el Plioceno-Pleistoceno fue caracterizado por la producción de rocas magmáticas contrastantes, incluidas riolitas altas en sílice, andesitas con señal tipo adaquita y basaltos alcalinos con firma tipo OIB. Las ignimbritas riolíticas ricas en sílice fueron formadas en un periodo de gran flujo magmático (flare-up) que ocurrió en este segmento del arco a 2.6 Ma. En este estudio se propone que este alto flujo magmático produjo un alto volumen de cumulatos basálticos fueron retenidos en la base de la corteza, facilitando la formación de piroxenitas granatíferas conocidas como arclogitas. Este alto flujo magmático, podría estar relacionado al aumento del ingreso de sedimentos dentro de la placa subducente, como se evidencia en el modelamiento isotópico. Por estudios anteriores se conoce que las arclogitas de este segmento del arco son más densas que el manto subyacente. En este estudio se propone que el vulcanismo monogenético con basaltos alcalinos del Pleistoceno en esta sección del arco, fueron formados por pequeños fragmentos delaminados “dripping” en vez de delaminación completa de la corteza inferior entre el manto astenosférico. Dos tipos de arclogitas se fundieron para generar este tipo de magmatismo, una piroxenita con granate y una piroxenita con granate y anfíbol. Los capítulos desarrollados en esta tesis muestran cómo la margen continental de la parte más norte de los Andes ha sido dinámica a través del Cenozoico. El orógeno colombiano, a diferencia de los Andes Centrales, donde el acortamiento tectónico controla el orógeno, está controlado principalmente por la acreción de bloques, tectónica de rumbo y el apilamiento magmático. El apilamiento magmático en esta sección del arco Andino fue quizás el factor más crítico en el control del espesor cortical y posterior remoción de su parte inferior más densa e inestable.DoctoradoDoctor en IngenieríaGeologíaÁrea Curricular de Materiales y Nanotecnología156 páginasapplication/pdfengUniversidad Nacional de ColombiaMedellín - Minas - Doctorado en Ingeniería - Ciencia y Tecnología de MaterialesFacultad de MinasUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaMagnetismoIsotoposCronología geológicaGeoquímicaMagmatismU-Pb and Ar-Ar GeochronologyGeochemistryIsotopesDripping,Northern AndesMagmatismoGeocronología U-Pb y Ar-ArGeoquímicaIsotoposMagmatism as a tracer of the cenozoic crustal evolution of the Northern AndesMagmatismo como un trazador de la evolución cortical cenozoica de los Andes del NorteTrabajo de grado - Doctoradoinfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_db06Texthttp://purl.org/redcol/resource_type/TDAcosta, J. 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Slab-rollback ignimbrite flare-ups in the southern Great Basin and other Cenozoic American arcs: A distinct style of arc volcanism. Geosphere, 12(4), 1097-1135. https://doi.org/10.1130/ges01285.1Best, M. G., Christiansen, E. H., Deino, A. L., Gromme, S., Hart, G. L., & Tingey, D. G. (2013). The 36-18 Ma Indian Peak-Caliente ignimbrite field and calderas, southeastern Great Basin, USA: multicyclic super-eruptions. Geosphere, 9(4), 864-950. https://doi.org/10.1130/GES00902.1Black, L. P., Kamo, S. L., Allen, C. M., Davis, D. W., Aleinikoff, J. N., Valley, J. W., Mundil, R., Campbell, I. H., Korsch, R. J., Williams, I. S., & Foudoulis, C. (2004). Improved 206Pb/238U microprobe geochronology by the monitoring of a trace-element-related matrix effect; SHRIMP, ID-TIMS, ELA-ICP-MS and oxygen isotope documentation for a series of zircon standards. 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Magmatism as a tracer of the cenozoic crustal evolution of the Northern Andes

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