Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia

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dc.contributor.advisorGalindo Amaya, Pedro Alejandro
dc.contributor.advisorCamargo Cortés, Guillermo Arturo
dc.contributor.authorVargas Vargas, Mayra Liseth
dc.coverage.regionMagdalena
dc.coverage.regionValle Medio del Magdalena
dc.date.accessioned2022-02-01T21:45:59Z
dc.date.available2022-02-01T21:45:59Z
dc.date.issued2021
dc.descriptionilustraciones, graficas, mapasspa
dc.description.abstractLa Falla Casabe se encuentra en el flanco occidental de la cuenca del Valle Medio del Magdalena (Colombia). Estudios anteriores presentan información estructural de la falla a nivel de reservorio, por lo que su evolución y estilos de deformación no habían sido estudiados en detalle hasta el momento. Este estudio integra la interpretación sísmica 3D de los volúmenes sísmicos CASABE PEÑAS BLANCAS 3D y LLANITO 3D cubriendo un área total de 212 Km2, brindando una oportunidad única de visualizar tridimensionalmente la terminación norte de una falla regional de rumbo en el subsuelo. Como resultado de la interpretación, se generan mapas estructurales en tiempo, mapas de espesor de unidades y gráficas de desplazamiento vertical y de intervalo, los cuales en conjunto permiten el análisis de los estilos estructurales y patrones de depositación en el área. Entre los estilos observados se encuentran evidencias de procesos de reactivación de fallas, así como de deformación de rumbo. Se identifican 9 segmentos de falla profundos (en la sección Cretácica) los cuales son reactivados y amalgamados por la deformación de rumbo durante el Cenozoico. Evidencias de la deformación de rumbo incluyen la ocurrencia de fallas normales con arreglo en-échelon, estructuras de pop-up y pull-apart, y terminaciones en cola de caballo. Con las geometrías identificadas, se genera un modelo esquemático de la Falla Casabe en el área de estudio, representando la variación tridimensional de estructuras asociadas a la falla. Así mismo, el análisis de los resultados permite identificar deformación previa a la Discordancia del Eoceno (Cretácico tardío–Paleoceno) y proponer que la deformación de rumbo ha sido activa desde el Eoceno tardío hasta el Reciente. (texto tomado en la fuente)spa
dc.description.abstractThe Casabe Fault is located in the western flank of the Middle Magdalena Basin (Colombia). Previous studies of the fault have shown structural information focused at reservoir level, and then its evolution and deformation styles had not been analyzed as yet. This study integrates the 3D seismic interpretation of the seismic volumes CASABE PEÑAS BLANCAS 3D and LLANITO 3D covering an area of 212 Km2, providing a unique opportunity to visualize three-dimensionally the northern tip of a regional strike-slip fault in the subsurface. As a result of the interpretation, time structural maps, time-thickness maps, together with vertical and interval displacement diagrams are generated. These allow the analysis of structural styles and depositional patterns in the area. The structural styles observed include fault reactivation processes and strike-slip deformation. Nine fault segments within the Cretaceous section are identified. These were reactivated and amalgamated by the strike-slip deformation during the Cenozoic. Evidence for strike-slip deformation includes the occurrence of en-échelon normal faults, pop-up and pull-apart structures, and horsetail terminations. A schematic model of the Casabe Fault is generated for the study area, representing the three-dimensional variation of structures associated to the fault plane. Likewise, the analysis of the results, allows identify deformation prior to the Eocene Unconformity (Late Cretaceous – Paleocene), and propose that the strike-slip deformation has been active since the late Eocene to the Recenteng
dc.description.degreelevelMaestríaspa
dc.description.degreenameMagíster en Ciencias - Geologíaspa
dc.description.researchareaGeología Estructuralspa
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/80847
dc.language.isospaspa
dc.publisherUniversidad Nacional de Colombiaspa
dc.publisher.branchUniversidad Nacional de Colombia - Sede Bogotáspa
dc.publisher.departmentDepartamento de Geocienciasspa
dc.publisher.facultyFacultad de Cienciasspa
dc.publisher.placeBogotá, Colombiaspa
dc.publisher.programBogotá - Ciencias - Maestría en Ciencias - Geologíaspa
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dc.rights.accessrightsinfo:eu-repo/semantics/openAccessspa
dc.rights.licenseAtribución-NoComercial-CompartirIgual 4.0 Internacionalspa
dc.rights.urihttp://creativecommons.org/licenses/by-nc-sa/4.0/spa
dc.subject.ddc550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaspa
dc.subject.otherHundimiento del suelo
dc.subject.proposalFalla Casabespa
dc.subject.proposalDeformación de rumbospa
dc.subject.proposalReactivación de fallasspa
dc.subject.proposalValle Medio del Magdalenaspa
dc.subject.proposalColombiaspa
dc.subject.proposalInterpretación sísmica 3Dspa
dc.subject.proposalCasabe Faulteng
dc.subject.proposalStrike-slip faultseng
dc.subject.proposalFault reactivationeng
dc.subject.proposalMiddle Magdalena Valleyeng
dc.subject.proposal3D seismic interpretationeng
dc.subject.unescoDeslizamiento de tierra
dc.subject.unescoSismo
dc.titleGeometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombiaspa
dc.title.translatedGeometry and evolution of the Casabe Fault in the Middle Magdalena Valley, Colombiaeng
dc.typeTrabajo de grado - Maestríaspa
dc.type.coarhttp://purl.org/coar/resource_type/c_bdccspa
dc.type.coarversionhttp://purl.org/coar/version/c_ab4af688f83e57aaspa
dc.type.contentTextspa
dc.type.driverinfo:eu-repo/semantics/masterThesisspa
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dc.type.versioninfo:eu-repo/semantics/acceptedVersionspa
dcterms.audience.professionaldevelopmentEstudiantesspa
dcterms.audience.professionaldevelopmentInvestigadoresspa
dcterms.audience.professionaldevelopmentPúblico generalspa
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