Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia

ilustraciones, mapas

Autores:: Buitrago Segura, Harold Steven

Tipo de recurso:

Fecha de publicación:: 2022

Institución:: Universidad Nacional de Colombia

Repositorio:: Universidad Nacional de Colombia

Idioma:: spa

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dc.title.spa.fl_str_mv	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
dc.title.translated.eng.fl_str_mv	Modeling of the lithospheric thermal field by the method of conservative finite differences applied around the area of the Eastern Cordillera , Colombia
title	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
spellingShingle	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia 550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur 530 - Física::536 - Calor Calentamiento global Calorimetría Global warming Calorimeters and calorimetry Campo térmico Flujo de calor Diferencias finitas Gradiente geotérmico Cordillera oriental Thermal field Heat flow Finite difference Geothermal gradient Eastern cordillera
title_short	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
title_full	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
title_fullStr	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
title_full_unstemmed	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
title_sort	Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia
dc.creator.fl_str_mv	Buitrago Segura, Harold Steven
dc.contributor.advisor.none.fl_str_mv	Vargas Jimenez, Carlos Alberto Neumann, Florian
dc.contributor.author.none.fl_str_mv	Buitrago Segura, Harold Steven
dc.contributor.researchgroup.spa.fl_str_mv	Cenit
dc.contributor.subjectmatterexpert.none.fl_str_mv	Contreras, Juan
dc.contributor.orcid.spa.fl_str_mv	Buitrago, Harold [0000-0002-0592-0370]
dc.contributor.cvlac.spa.fl_str_mv	Buitrago Segura, Harold Steven
dc.subject.ddc.spa.fl_str_mv	550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur 530 - Física::536 - Calor
topic	550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur 530 - Física::536 - Calor Calentamiento global Calorimetría Global warming Calorimeters and calorimetry Campo térmico Flujo de calor Diferencias finitas Gradiente geotérmico Cordillera oriental Thermal field Heat flow Finite difference Geothermal gradient Eastern cordillera
dc.subject.lemb.spa.fl_str_mv	Calentamiento global Calorimetría
dc.subject.lemb.eng.fl_str_mv	Global warming Calorimeters and calorimetry
dc.subject.proposal.spa.fl_str_mv	Campo térmico Flujo de calor Diferencias finitas Gradiente geotérmico Cordillera oriental
dc.subject.proposal.eng.fl_str_mv	Thermal field Heat flow Finite difference Geothermal gradient Eastern cordillera
description	ilustraciones, mapas
publishDate	2022
dc.date.issued.none.fl_str_mv	2022
dc.date.accessioned.none.fl_str_mv	2023-06-28T20:34:40Z
dc.date.available.none.fl_str_mv	2023-06-28T20:34:40Z
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	DataPaper Model Software Workflow
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/84096
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/84096 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	spa
language	spa
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Three-dimensional inverse modelling of the thermal structure and implications for lithospheric strength in Denmark and adjacent areas of Northwest Europe. Geophysical Journal International, 147(1), 141–154. https://doi.org/10.1046/j.0956-540X.2001.01528.x Gerya, T. (2010). Introduction to numerical geodynamic modelling. Cambrifge University Press. Hacker, B. R., Kelemen, P. B., & Behn, M. D. (2011). Differentiation of the continental crust by relamination. Earth and Planetary Science Letters, 307(3–4), 501–516. https://doi.org/10.1016/j.epsl.2011.05.024 Hacker, B. R., Kelemen, P. B., & Behn, M. D. (2015). Continental lower crust. Annual Review of Earth and Planetary Sciences, 43, 167–205. https://doi.org/10.1146/annurev-earth-050212-124117 Hamza, V. M., & Vieira, F. (2018). Global Heat Flow: New Estimates Using Digital Maps and GIS Techniques. International Journal of Terrestrial Heat Flow and Applications, 1(1), 6–13. https://doi.org/10.31214/ijthfa.v1i1.6 Hasterok, D., & Chapman, D. S. (2011). Heat production and geotherms for the continental lithosphere. Earth and Planetary Science Letters, 307(1–2), 59–70. https://doi.org/10.1016/j.epsl.2011.04.034 Hasterok, D., Gard, M., & Webb, J. (2017). On the radiogenic heat production of metamorphic, igneous, and sedimentary rocks. Geoscience Frontiers, 9(6), 1777–1794. https://doi.org/10.1016/j.gsf.2017.10.012 Hokstad, K., Tašárová, Z. A., Clark, S. A., Kyrkjebø, R., Duffaut, K., Fichler, C., & Wiik, T. (2017). Radiogenic heat production in the crust from inversion of gravity and magnetic data. Norwegian Journal of Geology, 97(3), 241–254. https://doi.org/10.17850/njg97-3-04 Horton, B. K., & Saylor, J. E. (2010). Resolving uplift of the using detrital zircon. July. https://doi.org/10.1130/GSATG76A.1 Jaupart, C., & Mareschal, J. C. (1999). The thermal structure and thickness of continental roots. Developments in Geotectonics, 24(C), 93–114. https://doi.org/10.1016/S0419-0254(99)80007-X Jaupart, C. 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Major and trace element composition of the depleted MORB mantle (DMM). Earth and Planetary Science Letters, 231(1–2), 53–72. https://doi.org/10.1016/j.epsl.2004.12.005 Zhang, L., Mao, X., & Lu, A. (2009). Experimental study on the mechanical properties of rocks at high temperature. Science in China, Series E: Technological Sciences, 52(3), 641–646. https://doi.org/10.1007/s11431-009-0063-y
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spelling	Reconocimiento 4.0 Internacionalhttp://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Vargas Jimenez, Carlos Albertob88c5098ce93a82d389779a59019f861Neumann, Floriane8dc334d15ea5cfedc49aea54db4f17eBuitrago Segura, Harold Steven9f2844a2ca5f233a5bd76ad4b9d3a417CenitContreras, JuanBuitrago, Harold [0000-0002-0592-0370]Buitrago Segura, Harold Steven2023-06-28T20:34:40Z2023-06-28T20:34:40Z2022https://repositorio.unal.edu.co/handle/unal/84096Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, mapasEn esta tesis se discretizó la ecuación de conducción-advección por el método de diferencias finitas conservativas y se escribió un código en Matlab que resuelve el campo de temperatura de la litosfera en 2D. Este código se validó comparando sus resultados con soluciones analíticas de algunos escenarios tectónicos sencillos en 1D y 2D reportadas en la literatura. La soluciones numéricas obtenidas concuerdan con las analíticas mostrando que se alcanzan diferencias menores a 1°C siempre que la discretización sea densa (>5000 nodos verticales). Los mejores resultados se obtienen en los casos en que no existen fuentes o sumideros de calor en el espacio modelado. Posteriormente, el código se empleó para resolver el campo térmico litosférico en la Cordillera Oriental de Colombia. Para constreñir las soluciones numéricas se utilizó la base de datos de gradiente geotérmico LogDB y algunas estimaciones de flujo de calor realizadas en la cuenca de Llanos Orientales. Los valores de parámetros materiales como la conductividad térmica, calor especifico, producción de calor radiogénico, etc., fueron tomados de la literatura para las rocas que afloran en el área e inferidos para la corteza y manto superior. Las condiciones de frontera que ajustan mejor a los datos en superficie sugieren la ocurrencia de un basamento enriquecido en elementos radiactivos que sería una fuente importante de calor (1.6 – 3 μWm-3) al este del sistema de fallas de Guaicaramo en donde se han documentado sistemas geotérmicos activos. El flujo de calor astenosferico modelado oscila entre 15-25 mWm-2 excepto sobre la Cordillera Oriental al norte del desgarre de Caldas en donde el flujo necesario para elevar el límite litosfera-astenosfera hasta 70-80 km requiere de un flujo astenosferico adicional de 15-20 mWm-2 (30-45 mWm-2 total). El flujo de calor adicional podría deberse a advección por flujo mantélico no contemplado en la simulación o a la ocurrencia de procesos como el calentamiento viscoso causado por cizalla (viscous heating). (Texto tomado de la fuente)In this thesis, the conduction-advection equation was discretized by the conservative finite difference method, and a code was written in MATLAB that solves the temperature field of the lithosphere in 2D. This code was validated by comparing its results with analytical solutions of some simple 1D and 2D tectonic scenarios reported in the literature. The numerical solutions obtained agree with the analytical ones, showing that differences of less than 1°C are reached as long as the discretization is dense (>5000 vertical nodes). The best results are obtained in cases where there are no heat sources or sinks in the modeled space. Subsequently, the code was used to solve the lithospheric thermal field in the Eastern Cordillera of Colombia. To constrain the numerical solutions, the LogDB geothermal gradient database and some heat flow estimates made in the Llanos Orientales basin were used. The values of material parameters such as thermal conductivity, specific heat, radiogenic heat production, etc., were taken from the literature for the rocks that outcrop in the area and inferred for the crust and upper mantle. The boundary conditions that best fit the surface data suggest the occurrence of a basement enriched in radioactive elements that would be an important source of heat (1.6 – 3 μWm-3) to the east of the Guaicaramo fault system where active geothermal systems have been documented. The modeled asthenospheric heat flow ranges in 15-25 mWm-2 except over the Eastern Cordillera north of the Caldas tear, where heat flow needed to raise the lithosphere-asthenosphere boundary to 70-80 km requires higher values (30-45mW). The additional heat flow could be due to advection by mantle flow not considered in the simulation or to the occurrence of processes such as viscous heating.MaestríaMagister en Ciencias GeofisicaSe relizo un modelado numerico bidimensional del campo termico conductivo en la litosfera y se calibro con datos de gradiente geotermico y flujo de calor de Colombia.Campo termico litosfericoflujo de calorxiv, 92 páginasapplication/pdfspaUniversidad Nacional de ColombiaBogotá - Ciencias - Maestría en Ciencias - GeofísicaFacultad de CienciasBogotá,ColombiaUniversidad Nacional de Colombia - Sede Bogotá550 - Ciencias de la tierra::558 - Ciencias de la tierra de América del Sur530 - Física::536 - CalorCalentamiento globalCalorimetríaGlobal warmingCalorimeters and calorimetryCampo térmicoFlujo de calorDiferencias finitasGradiente geotérmicoCordillera orientalThermal fieldHeat flowFinite differenceGeothermal gradientEastern cordilleraModelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, ColombiaModeling of the lithospheric thermal field by the method of conservative finite differences applied around the area of the Eastern Cordillera , ColombiaTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionDataPaperModelSoftwareWorkflowhttp://purl.org/redcol/resource_type/TMColombiaAlfaro, C., Alvarado, I., & Manrique, A. 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Science in China, Series E: Technological Sciences, 52(3), 641–646. https://doi.org/10.1007/s11431-009-0063-yEstudiantesInvestigadoresPúblico generalORIGINAL1024509176.2023.pdf1024509176.2023.pdfTesis de Maestría en Ciencias - Geofísicaapplication/pdf4623555https://repositorio.unal.edu.co/bitstream/unal/84096/2/1024509176.2023.pdfdfea21049e9b8c7f96565c5e628d54acMD52LICENSElicense.txtlicense.txttext/plain; charset=utf-85879https://repositorio.unal.edu.co/bitstream/unal/84096/1/license.txteb34b1cf90b7e1103fc9dfd26be24b4aMD51THUMBNAIL1024509176.2023.pdf.jpg1024509176.2023.pdf.jpgGenerated Thumbnailimage/jpeg5660https://repositorio.unal.edu.co/bitstream/unal/84096/3/1024509176.2023.pdf.jpgc830489dfa1fdf88f97c3c0970972cd0MD53unal/84096oai:repositorio.unal.edu.co:unal/840962023-08-10 23:04:18.288Repositorio Institucional Universidad Nacional de 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Modelado del campo térmico litosférico por el método de diferencias finitas conservativas aplicado en el área de la Cordillera Oriental, Colombia

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