Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia

Los Llanos Orientales de Colombia corresponden a un sistema de cuenca antepaís que registró el inicio del pulso tectónico más reciente a partir del Mioceno (Campos, 2011) influenciado en gran medida por la colisión y acreción del bloque Chocó en el Noroeste de Suramérica en el Mioceno medio (Vargas...

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Autores:
Alva Carmona, Maria Rosa
Tipo de recurso:
Fecha de publicación:
2020
Institución:
Universidad Nacional de Colombia
Repositorio:
Universidad Nacional de Colombia
Idioma:
spa
OAI Identifier:
oai:repositorio.unal.edu.co:unal/79347
Acceso en línea:
https://repositorio.unal.edu.co/handle/unal/79347
Palabra clave:
550 - Ciencias de la tierra
Modelo Flexural 3D
Cuenca antepaís
Isostasia
Espesor elástico
Rigidez de la Litosfera
Evolución tectonoestratigráfica
Llanos Orientales de Colombia
3D Flexural Modeling
Foreland basin
Isostasy
Elastic thickness
Lithosphere rigidity
Tectonostratigraphic evolution
Eastern Llanos
Colombia
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openAccess
License
Atribución-NoComercial-SinDerivadas 4.0 Internacional
id UNACIONAL2_21158cbaae77d60d33c30fb19ea406c7
oai_identifier_str oai:repositorio.unal.edu.co:unal/79347
network_acronym_str UNACIONAL2
network_name_str Universidad Nacional de Colombia
repository_id_str
dc.title.spa.fl_str_mv Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
title Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
spellingShingle Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
550 - Ciencias de la tierra
Modelo Flexural 3D
Cuenca antepaís
Isostasia
Espesor elástico
Rigidez de la Litosfera
Evolución tectonoestratigráfica
Llanos Orientales de Colombia
3D Flexural Modeling
Foreland basin
Isostasy
Elastic thickness
Lithosphere rigidity
Tectonostratigraphic evolution
Eastern Llanos
Colombia
title_short Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
title_full Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
title_fullStr Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
title_full_unstemmed Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
title_sort Modelado Flexural 3D de la cuenca Llanos Orientales de Colombia
dc.creator.fl_str_mv Alva Carmona, Maria Rosa
dc.contributor.advisor.spa.fl_str_mv Vargas J., Carlos A.
Bayona, Germán
dc.contributor.author.spa.fl_str_mv Alva Carmona, Maria Rosa
dc.subject.ddc.spa.fl_str_mv 550 - Ciencias de la tierra
topic 550 - Ciencias de la tierra
Modelo Flexural 3D
Cuenca antepaís
Isostasia
Espesor elástico
Rigidez de la Litosfera
Evolución tectonoestratigráfica
Llanos Orientales de Colombia
3D Flexural Modeling
Foreland basin
Isostasy
Elastic thickness
Lithosphere rigidity
Tectonostratigraphic evolution
Eastern Llanos
Colombia
dc.subject.proposal.none.fl_str_mv Modelo Flexural 3D
Cuenca antepaís
Isostasia
Espesor elástico
Rigidez de la Litosfera
Evolución tectonoestratigráfica
Llanos Orientales de Colombia
3D Flexural Modeling
Foreland basin
Isostasy
Elastic thickness
Lithosphere rigidity
Tectonostratigraphic evolution
Eastern Llanos
Colombia
description Los Llanos Orientales de Colombia corresponden a un sistema de cuenca antepaís que registró el inicio del pulso tectónico más reciente a partir del Mioceno (Campos, 2011) influenciado en gran medida por la colisión y acreción del bloque Chocó en el Noroeste de Suramérica en el Mioceno medio (Vargas & Mann, 2013). La deformación litosférica resultante fue representada mediante el primer modelo Flexural 3D de la cuenca de antepaís Llanos Orientales de Colombia, discretizado en 5 intervalos de tiempo desde el Mioceno medio al Presente. Con este trabajo se pretende ampliar el conocimiento en cuanto a la evolución tectonoestratigráfica de la cuenca de antepaís, mediante la identificación de las variaciones de espesor elástico (Te), modelamiento de la ubicación de las depozonas y predicciones de la configuración y movimiento del orógeno (Cordillera Oriental). Se empleó el código FLEX3DV, desarrollado en MatLab por Cardozo (2009). Este código se basa en una solución por diferencias finitas centradas a la ecuación de deflexión de una placa de espesor variable (Ventsel & Krauthammer, 2001). En el modelado Flexural 3D se integraron datos de estudios previos (e.g. mapas de espesores, secciones estructurales evolutivas). Los resultados consisten en mapas que muestran áreas de levantamiento y subsidencia del sistema Cordillera Oriental- Llanos Orientales. Estos mapas fueron comparados con modelos flexurales 2D previos realizados en el área de Los Llanos y en cuencas de antepaís adyacentes. Los modelados flexurales 3D para cada intervalo de tiempo permitieron ver una una estrecha relación entre la dirección de desplazamiento de la onda flexural modelada y los diferentes procesos del bloque que subduce desde el Mioceno medio al Presente.
publishDate 2020
dc.date.issued.spa.fl_str_mv 2020
dc.date.accessioned.spa.fl_str_mv 2021-03-10T14:39:26Z
dc.date.available.spa.fl_str_mv 2021-03-10T14:39:26Z
dc.type.spa.fl_str_mv Trabajo de grado - Maestría
dc.type.driver.spa.fl_str_mv info:eu-repo/semantics/masterThesis
info:eu-repo/semantics/masterThesis
dc.type.version.spa.fl_str_mv info:eu-repo/semantics/acceptedVersion
dc.type.coarversion.spa.fl_str_mv http://purl.org/coar/version/c_fa2ee174bc00049f
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/79347
url https://repositorio.unal.edu.co/handle/unal/79347
dc.language.iso.spa.fl_str_mv spa
language spa
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dc.format.extent.spa.fl_str_mv 1 recurso en línea (133 páginas)
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dc.publisher.spa.fl_str_mv Universidad Nacional de Colombia
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dc.publisher.branch.spa.fl_str_mv Universidad Nacional de Colombia - Sede Bogotá
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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_abf2Vargas J., Carlos A.a6ff1eda-1201-48ce-95f3-d8daf4a5e9afBayona, Germán9b0d4143-1d62-4af2-88bc-63fb9d65c44bAlva Carmona, Maria Rosa51172264-23f4-4b91-9221-73b6f24ed1662021-03-10T14:39:26Z2021-03-10T14:39:26Z2020https://repositorio.unal.edu.co/handle/unal/79347Los Llanos Orientales de Colombia corresponden a un sistema de cuenca antepaís que registró el inicio del pulso tectónico más reciente a partir del Mioceno (Campos, 2011) influenciado en gran medida por la colisión y acreción del bloque Chocó en el Noroeste de Suramérica en el Mioceno medio (Vargas & Mann, 2013). La deformación litosférica resultante fue representada mediante el primer modelo Flexural 3D de la cuenca de antepaís Llanos Orientales de Colombia, discretizado en 5 intervalos de tiempo desde el Mioceno medio al Presente. Con este trabajo se pretende ampliar el conocimiento en cuanto a la evolución tectonoestratigráfica de la cuenca de antepaís, mediante la identificación de las variaciones de espesor elástico (Te), modelamiento de la ubicación de las depozonas y predicciones de la configuración y movimiento del orógeno (Cordillera Oriental). Se empleó el código FLEX3DV, desarrollado en MatLab por Cardozo (2009). Este código se basa en una solución por diferencias finitas centradas a la ecuación de deflexión de una placa de espesor variable (Ventsel & Krauthammer, 2001). En el modelado Flexural 3D se integraron datos de estudios previos (e.g. mapas de espesores, secciones estructurales evolutivas). Los resultados consisten en mapas que muestran áreas de levantamiento y subsidencia del sistema Cordillera Oriental- Llanos Orientales. Estos mapas fueron comparados con modelos flexurales 2D previos realizados en el área de Los Llanos y en cuencas de antepaís adyacentes. Los modelados flexurales 3D para cada intervalo de tiempo permitieron ver una una estrecha relación entre la dirección de desplazamiento de la onda flexural modelada y los diferentes procesos del bloque que subduce desde el Mioceno medio al Presente.The Eastern Llanos of Colombia foreland basin system recorded the beginning of the most recent tectonic pulse from the Miocene (Campos, 2011). This tectonic pulse was mainly triggered by the Panama Arc accretion in Northwestern South America in the Middle Miocene (Vargas & Mann, 2013). The resulting lithospheric deformation was represented by the first 3D Flexural modeling of the Llanos Orientales basin, discretized in 5 time intervals from the Middle Miocene to the Present. This work aims to expand knowledge regarding the tectonostratigraphic evolution of the foreland basin, by identifying the variations in elastic thickness (Te), modeling the location of the depozones and making predictions about how the orogen (Eastern Cordillera) developed in the last 16 Ma. 3D flexural models were generated by using the code FLEX3DV, developed in MatLab by Cardozo (2009). This code solves the flexural equation by a centered finite differences solution for a variable thickness plate (Ventsel & Krauthammer, 2001). Data from previous studies were integrated into 3D flexural modeling (e.g. thickness maps, balanced cross-sections). The results consist of maps showing uplift and subsidence areas in the Eastern Cordillera-Eastern Llanos region. These maps were compared with previous 2D flexural model results in the study area and in adjacent foreland basins. 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