Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes
ilustraciones, diagramas, tablas
- Autores:
-
León Vasco, Santiago
- Tipo de recurso:
- Doctoral thesis
- Fecha de publicación:
- 2022
- Institución:
- Universidad Nacional de Colombia
- Repositorio:
- Universidad Nacional de Colombia
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.unal.edu.co:unal/81688
- Palabra clave:
- 550 - Ciencias de la tierra
620 - Ingeniería y operaciones afines::629 - Otras ramas de la ingeniería
Cuencas hidrográficas
Watersheds
Rocas - Análisis
Forearc basins
Northern Andes
Arc-continent collision
Atrato Basin
Sedimentary provenance
Tectonostratigraphy
Cuencas antearco
Andes del Norte
Colisión arco-continente
Cuenca Atrato
Procedencia sedimentaria
Tectonoestratigrafía
- Rights
- openAccess
- License
- Atribución-NoComercial-SinDerivadas 4.0 Internacional
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Universidad Nacional de Colombia |
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| dc.title.eng.fl_str_mv |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| dc.title.translated.spa.fl_str_mv |
Evolución de cuencas de antearco en respuesta a un régimen de subducción cambiante: Registro geológico Neógeno al Reciente del noroccidente de los Andes Colombianos |
| title |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| spellingShingle |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes 550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::629 - Otras ramas de la ingeniería Cuencas hidrográficas Watersheds Rocas - Análisis Forearc basins Northern Andes Arc-continent collision Atrato Basin Sedimentary provenance Tectonostratigraphy Cuencas antearco Andes del Norte Colisión arco-continente Cuenca Atrato Procedencia sedimentaria Tectonoestratigrafía |
| title_short |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| title_full |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| title_fullStr |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| title_full_unstemmed |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| title_sort |
Forearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian Andes |
| dc.creator.fl_str_mv |
León Vasco, Santiago |
| dc.contributor.advisor.none.fl_str_mv |
Monsalve Mejía, Gaspar |
| dc.contributor.author.none.fl_str_mv |
León Vasco, Santiago |
| dc.subject.ddc.spa.fl_str_mv |
550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::629 - Otras ramas de la ingeniería |
| topic |
550 - Ciencias de la tierra 620 - Ingeniería y operaciones afines::629 - Otras ramas de la ingeniería Cuencas hidrográficas Watersheds Rocas - Análisis Forearc basins Northern Andes Arc-continent collision Atrato Basin Sedimentary provenance Tectonostratigraphy Cuencas antearco Andes del Norte Colisión arco-continente Cuenca Atrato Procedencia sedimentaria Tectonoestratigrafía |
| dc.subject.lemb.none.fl_str_mv |
Cuencas hidrográficas Watersheds Rocas - Análisis |
| dc.subject.proposal.eng.fl_str_mv |
Forearc basins Northern Andes Arc-continent collision Atrato Basin Sedimentary provenance Tectonostratigraphy |
| dc.subject.proposal.spa.fl_str_mv |
Cuencas antearco Andes del Norte Colisión arco-continente Cuenca Atrato Procedencia sedimentaria Tectonoestratigrafía |
| description |
ilustraciones, diagramas, tablas |
| publishDate |
2022 |
| dc.date.accessioned.none.fl_str_mv |
2022-07-07T15:20:19Z |
| dc.date.available.none.fl_str_mv |
2022-07-07T15:20:19Z |
| dc.date.issued.none.fl_str_mv |
2022 |
| dc.type.spa.fl_str_mv |
Trabajo de grado - Doctorado |
| dc.type.driver.spa.fl_str_mv |
info:eu-repo/semantics/doctoralThesis |
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info:eu-repo/semantics/acceptedVersion |
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http://purl.org/coar/resource_type/c_db06 |
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Text |
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http://purl.org/redcol/resource_type/TD |
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http://purl.org/coar/resource_type/c_db06 |
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acceptedVersion |
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https://repositorio.unal.edu.co/handle/unal/81688 |
| 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/81688 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.references.spa.fl_str_mv |
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Thermochronology and tectonics of the Central and Western Cordilleras of Colombia: Early Cretaceous–Tertiary evolution of the Northern Andes. Lithos 160–161, 228–249. https://doi.org/10.1016/j.lithos.2012.12.008 Villagómez, D., Spikings, R.A., Magna, T., Kammer, A., Winkler, W., Beltrán, A., 2011. Geochronology, geochemistry and tectonic evolution of the Western and Central cordilleras of Colombia. Lithos 125, 875–896. https://doi.org/10.1016/j.lithos.2011.05.003 Viveen, W., Schlunegger, F., 2018. Prolonged extension and subsidence of the Peruvian forearc during the Cenozoic. Tectonophysics 730, 48–62. https://doi.org/10.1016/j.tecto.2018.02.018 Vogt, K., Gerya, T. V., 2014. From oceanic plateaus to allochthonous terranes: Numerical modelling. Gondwana Res. 25, 494–508. https://doi.org/10.1016/j.gr.2012.11.002 von Eynatten, H., Dunkl, I., 2012. Assessing the sediment factory: The role of single grain analysis. Earth-Science Rev. 115, 97–120. https://doi.org/10.1016/j.earscirev.2012.08.001 von Huene, R., Ranero, C.R., Vannucchi, P., 2004. Generic model of subduction erosion. Geology 32, 913–916. https://doi.org/10.1130/G20563.1 von Huene, R., Scholl, D.W., 1991. Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust. Rev. Geophys. 29, 279–316. https://doi.org/10.1029/91RG00969 Wagner, L.S., Jaramillo, J.S., Ramírez-Hoyos, L.F., Monsalve, G., Cardona, A., Becker, T.W., 2017. Transient slab flattening beneath Colombia. Geophys. Res. Lett. 44. https://doi.org/10.1002/2017GL073981 Wagreich, M., 1995. Subduction erosion and Late Cretaceous subsidence along the northern Austroalpine margin (Eastern Alps, Austria). Tectonophysics 242, 63–78. https://doi.org/10.1016/0040-1951(94)00151-X Wang, J.-G., Hu, X., Garzanti, E., BouDagher-Fadel, M.K., Liu, Z.-C., Li, J., Wu, F.-Y., 2020. From extension to tectonic inversion: Mid-Cretaceous onset of Andean-type orogeny in the Lhasa block and early topographic growth of Tibet. Geol. Soc. Am. Bull. 132, 2432–2454. https://doi.org/10.1130/B35314.1 Wang, K., He, J., 1999. Mechanics of low-stress forearcs: Nankai and Cascadia. J. Geophys. Res. Solid Earth 104, 15191–15205. https://doi.org/10.1029/1999JB900103 Weber, M., Cardona, A., Paniagua, F., Cordani, U., Sepúlveda, L., Wilson, R., 2009. The Cabo de la Vela Mafic-Ultramafic Complex, Northwestern Colombian Caribbean region: a record of multistage evolution of a Late Cretaceous intra-oceanic arc, in: James, K.H., Lorente, M.A., Pindell, J.L. (Eds.), The Origin and Evolution of the Caribbean Plate, Geological Society, London, Special Publications, 328. pp. 549–568. https://doi.org/10.1144/SP328.22 Weber, M., Gómez-Tapias, J., Cardona, A., Duarte, E., Pardo-Trujillo, A., Valencia, V., 2015. Geochemistry of the Santa Fé Batholith and Buriticá Tonalite in NW Colombia - Evidence of subduction initiation beneath the Colombian Caribbean Plateau. J. South Am. Earth Sci. 62, 257–274. https://doi.org/10.1016/j.jsames.2015.04.002 Wegner, W., Wörner, G., Harmon, R.S., Jicha, B.R., 2011. Magmatic history and evolution of the Central American Land Bridge in Panama since Cretaceous times. Geol. Soc. Am. Bull. 123, 703–724. https://doi.org/10.1130/B30109.1 Whattam, S.A., Montes, C., Mcfadden, R.R., Cardona, A., Ramirez, D., Valencia, V., 2012. Age and origin of earliest adakitic-like magmatism in Panama: Implications for the tectonic evolution of the Panamanian magmatic arc system. Lithos 142–143, 226–244. https://doi.org/10.1016/j.lithos.2012.02.017 Whattam, S.A., Montes, C., Stern, R.J., 2020. Early central American forearc follows the subduction initiation rule. Gondwana Res. 79, 283–300. https://doi.org/10.1016/j.gr.2019.10.002 Whattam, S.A., Stern, R.J., 2015. Late Cretaceous plume-induced subduction initiation along the southern margin of the Caribbean and NW South America: The first documented example with implications for the onset of plate tectonics. Gondwana Res. 27, 38–63. https://doi.org/10.1016/j.gr.2014.07.011 Wise, D.U., Funicello, R., Parotto, M., Salvini, F., 1985. Topographic lineament swarms: Clues to their origin from domain analysis of Italy. Geol. Soc. Am. Bull. 96, 952–967. https://doi.org/10.1130/0016-7606(1985)96<952:TLSCTT>2.0.CO;2 Wright, J.E., Wyld, S.J., 2011. Late Cretaceous subduction initiation on the eastern margin of the Caribbean-Colombian Oceanic Plateau: One Great Arc of the Caribbean (?). Geosphere 7, 468–493. https://doi.org/10.1130/GES00577.1 Xie, X., Heller, P.L., 2009. Plate tectonics and basin subsidence history. Bull. Geol. Soc. Am. 121, 55–64. https://doi.org/10.1130/B26398.1 Yarce, J., Monsalve, G., Becker, T.W., Cardona, A., Poveda, E., Alvira, D., Ordoñez-Carmona, O., 2014. 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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. J. South Am. Earth Sci. 112, 103557. https://doi.org/10.1016/j.jsames.2021.103557 Zapata, G., 2000. Geología de las planchas 163 Nuquí, 164 Quibdó, 183 Coquí y 184 Lloró, Departamento del Chocó. Escala 1:100.000. Memoria Explicativa. Zapata, S., Cardona, A., Jaramillo, J.S., Patiño, A., Valencia, V., León, S., Mejía, D., Pardo-Trujillo, A., Castañeda, J.P., 2019. Cretaceous extensional and compressional tectonics in the Northwestern Andes, prior to the collision with the Caribbean oceanic plateau. Gondwana Res. 66, 207–226. https://doi.org/10.1016/j.gr.2018.10.008 Zapata, S., Patiño, A., Cardona, A., Parra, M., Valencia, V., Reiners, P., Oboh-Ikuenobe, F., Genezini, F., 2020. Bedrock and detrital zircon thermochronology to unravel exhumation histories of accreted tectonic blocks: An example from the Western Colombian Andes. J. South Am. Earth Sci. 103, 102715. https://doi.org/10.1016/j.jsames.2020.102715 Zhu, D.-C., Wang, Q., Cawood, P.A., Zhao, Z.-D., Mo, X.-X., 2017. Raising the Gangdese Mountains in southern Tibet. J. Geophys. Res. Solid Earth 122, 214–223. https://doi.org/10.1002/2016JB013508 Zindler, A., Hart, S., 1986. Chemical geodynamics. Annu. Rev. Earth Planet. Sci. 14, 493–571. https://doi.org/10.1146/annurev.ea.14.050186.002425 |
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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_abf2Monsalve Mejía, Gaspar24932fa3561948cfb9d8ea2e55e6c7a8600León Vasco, Santiago6b6ddf33766e54bc8bdccece7ce650a22022-07-07T15:20:19Z2022-07-07T15:20:19Z2022https://repositorio.unal.edu.co/handle/unal/81688Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, diagramas, tablasThe growth of accretionary orogens, such as the northern Andes, involves both subduction-related tectonics and the collision of exotic terranes, including oceanic plateaus and island arcs. These contrasting tectonic regimes control the spatiotemporal evolution of deformational patterns and topography, whose signal is preserved in the tectonostratigraphic record of marginal basins, which is particularly true for forearc systems. This work presents a detailed geochronological and compositional characterization of Cretaceous magmatic rocks and Neogene strata of the northern Colombian forearc basin (Atrato Basin), which record the long-term evolution of the northwesternmost Andean region, since the early interactions with the Caribbean plate to the most recent shallow subduction of the Nazca plate. New petrochronological data from the Cupica and Tribugá gulfs allowed the recognition of a previously undocumented Upper-Cretaceous arc-related magmatic unit, which likely represents the earliest activity of the intra-oceanic Central American arc and the coeval island arc nowadays exposed along the north-Andean Western Cordillera. The collision of the latter and its plateau-like basement caused a major topographic uplift of the Colombian Central Cordillera during the Late Cretaceous-Paleocene, as suggested by new paleoelevation estimations presented in this work. Such collisional episode marked the early constitution of the northwestern Colombian forearc, whose evolution was subsequently controlled by the Neogene transition from the collision of the Central American arc and the subduction of the Nazca plate. A comprehensive tectonostratigraphic analysis of the Neogene infill of the Atrato Basin allowed identifying three main tectonic phases, which drove changes in the configuration of source areas and the depositional settings. First, the collision of the Central American arc against northwestern South America was recorded by the accumulation in a tectonically active back-arc basin of Oligocene-middle Miocene deep-marine strata sourced by both colliding domains. The advance of the collision triggered basin inversion and shallowing of accumulation depths during the middle Miocene, as well as accelerated erosional exhumation of the continental paleomargin and increased siliciclastic input to suture-related and the colliding back-arc basin. Second, the transition from collision to the subduction of the Nazca plate during the middle-late Miocene caused the formation of a post-collisional arc in northwestern Colombia, as well as the initial topographic uplift of the newly established forearc basin (former allochthonous back-arc) nearby the suture zone. This was accompanied by a major shallowing of accumulation depths and a dramatic change in the detrital signal of forearc deposits, which were isolated from continental source areas (i.e. Western Cordillera) by newly uplifted ranges. Finally, the late Miocene flattening of the subducting Nazca slab beneath northern Colombia caused widespread deformation that drove the uplift of the outer forearc high, represented by the coastal Baudó Range, and the establishment of the modern physiographic configuration. This episode led to the fragmentation of the forearc basin into an outer (coastal) and inner (inland) segments and strong reworking of older strata, as suggested by the provenance of late Miocene to Pliocene rocks accumulated in high-energy fluvial environments. The pulsated nature of Miocene mountain building along the northwesternmost Andean forearc, as a consequence of interspersed collisional and subduction-related tectonics, seemingly played a major role in the biogeographic evolution of the region and the constitution of the modern extremely humid tropical rainforest that hosts a biodiversity hotspot. This work allowed proving how valuable the tectonostratigraphic record of forearc basins and the surrounding mountain ranges is to disentangle the effects of a changing subduction system on the upper-plate landscape evolution, which, as demonstrated in this work, could be successfully studied through a combination of petrochronological, stratigraphic and structural analysesEl crecimiento de orógenos acrecionarios como los Andes del norte, involucra procesos tectónicos relacionados con subducción, así como la colisión de terrenos exóticos, incluyendo plateaux oceánicos y arcos de islas. Estos regímenes tectónicos contrastantes controlan la evolución espaciotemporal de los patrones de deformación y la topografía, cuya señal es preservada en el registro tectonoestratigráfico de las cuencas marginales, lo cual es particularmente cierto para sistemas de antearco. Este trabajo presenta una caracterización geocronológica y composicional detallada de las rocas magmáticas Cretácicas y sedimentos Neógenos del antearco norte de Colombia (Cuenca Atrato), las cuales registran la evolución de largo plazo de la región más noroccidental de los Andes, desde las interacciones tempranas con la placa Caribe hasta la más reciente subducción plana de la placa de Nazca. Nuevos datos petrocronológicos de sedimentos modernos de los golfos de Cupica y Tribugá permitieron reconocer una unidad magmática del Cretácico Tardío afín con un arco de islas que no había sido previamente documentada, la cual podría representar la actividad más temprana del arco Centro Americano y el arco de islas ahora expuesto a lo largo de la Cordillera Occidental de los Andes del norte. La colisión de este último, en conjunto con su basamento de tipo plateau, durante el Cretácico Tardío-Paleoceno, causó un importante levantamiento topográfico de la Cordillera Central Colombiana, como lo sugieren nuevas estimaciones de paleoelevación presentadas en este trabajo. Este episodio colisional marcó la conformación temprana del antearco noroccidental Colombiano, cuya evolución fue subsecuentemente controlada por la transición Neógena de colisión del arco Centro Americano y la subducción de la placa de Nazca. Un análisis tectonoestratigráfico integral del relleno Neógeno de la Cuenca Atrato permitió identificar tres fases tectónicas principales, las cuales detonaron cambios en la configuración de las áreas fuente y de los ambientes deposicionales. Primero, la colisión del arco Centro Americano con el noroccidente de Suramérica fue registrado por la acumulación, en una cuenca tras-arco tectónicamente activa, de rocas marinas profundas del Oligoceno-Mioceno medio con procedencia de ambos dominios en colisión. El avance del evento colisional detonó la inversión de la cuenca y la somerización de las profundidades de acumulación durante el Mioceno Medio, así como la exhumación por erosión acelerada de la paleomargen continental y el incremento del flujo siliciclástico hacia la cuenca de sutura y la cuenca de tras-arco en colisión. Segundo, la transición de colisión a subducción de la placa de Nazca durante el Mioceno medio-tardío causó la formación de un arco poscolisional en el noroccidente de Colombia, y también el levantamiento topográfico inicial de la recientemente establecida cuenca de antearco (antes tras-arco alóctono) en cercanías a la zona de sutura. Esto fue acompañado por una somerización importante de los ambientes de acumulación y un cambio dramático en la señal detrítica de los depósitos de antearco, los cuales fueron aislados de fuentes continentales (i.e. Cordillera Occidental) por montañas recientemente levantadas. Finalmente, el aplanamiento de la losa subducente de la placa de Nazca por debajo del norte de Colombia causó deformación ampliamente distribuida y condujo al levantamiento del alto externo del antearco, representado por la Serranía de Baudó, y al establecimiento de las condiciones fisiográficas modernas. Este episodio llevó a la fragmentación de la cuenca de antearco en un segmento externo (costero) y uno interno (continental), así como al fuerte retrabajamiento de rocas más antiguas, como lo sugiere la procedencia de rocas del Mioceno tardío al Plioceno acumuladas en ambientes fluviales de alta energía. La naturaleza episódica de la construcción de montañas durante el Mioceno a lo largo del antearco más noroccidental de los Andes, como consecuencia de tectónica colisional y de subducción, jugó, aparentemente, un papel importante en la evolución biogeográfica de la región y en la constitución del bosque tropical extremadamente húmedo de la actualidad, el cual hospeda un punto caliente de biodiversidad. Este trabajo permitió probar lo valioso que es el registro tectonoestratigráfico de las cuencas de antearco y las cadenas de montaña adyacentes para revelar los efectos de un sistema de subducción cambiante en la evolución del paisaje de la placa superior. Esto, como pudo demostrarse en este trabajo, puede ser exitosamente estudiado a través de la integración de análisis petrocronológicos, estratigráficos y estructurales. (Texto tomado de la fuente)DoctoradoDoctor en IngenieríaGeodinámicaÁrea Curricular de Materiales y Nanotecnologíaxviii, 170 páginasapplication/pdfengUniversidad Nacional de ColombiaMedellín - Minas - Doctorado en Ingeniería - Ciencia y Tecnología de MaterialesDepartamento de Materiales y MineralesFacultad de MinasMedellín, ColombiaUniversidad Nacional de Colombia - Sede Medellín550 - Ciencias de la tierra620 - Ingeniería y operaciones afines::629 - Otras ramas de la ingenieríaCuencas hidrográficasWatershedsRocas - AnálisisForearc basinsNorthern AndesArc-continent collisionAtrato BasinSedimentary provenanceTectonostratigraphyCuencas antearcoAndes del NorteColisión arco-continenteCuenca AtratoProcedencia sedimentariaTectonoestratigrafíaForearc basin evolution in response to a changing subduction system: Neogene to Recent geological record of the northwestern Colombian AndesEvolución de cuencas de antearco en respuesta a un régimen de subducción cambiante: Registro geológico Neógeno al Reciente del noroccidente de los Andes ColombianosTrabajo de grado - Doctoradoinfo:eu-repo/semantics/doctoralThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_db06Texthttp://purl.org/redcol/resource_type/TDAizprua, C., Witt, C., Johansen, S.E., Barba, D., 2019. 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Sci. 14, 493–571. https://doi.org/10.1146/annurev.ea.14.050186.002425Smithsonian Tropical Research InstituteFundación para la Promoción de la Investigación y la Tecnología - Banco de la República de ColombiaAsociación de Geólogos y Geofísicos del Petróleo y Corporación Geológica AresBibliotecariosEstudiantesInvestigadoresMaestrosORIGINAL1152439167.2022.pdf1152439167.2022.pdfTesis de Doctorado en Ingeniería - Ciencia y Tecnología de Materialesapplication/pdf8263320https://repositorio.unal.edu.co/bitstream/unal/81688/1/1152439167.2022.pdf671beb29ce1ebd5e544fd5f6e2f738c5MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-84074https://repositorio.unal.edu.co/bitstream/unal/81688/4/license.txt8153f7789df02f0a4c9e079953658ab2MD54THUMBNAIL1152439167.2022.pdf.jpg1152439167.2022.pdf.jpgGenerated Thumbnailimage/jpeg5016https://repositorio.unal.edu.co/bitstream/unal/81688/5/1152439167.2022.pdf.jpgae51f04f79fd9477b973691bff897063MD55unal/81688oai:repositorio.unal.edu.co:unal/816882023-10-20 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