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

ilustraciones, graficas, mapas

Autores:: Vargas Vargas, Mayra Liseth

Tipo de recurso:

Fecha de publicación:: 2021

Institución:: Universidad Nacional de Colombia

Repositorio:: Universidad Nacional de Colombia

Idioma:: spa

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dc.title.spa.fl_str_mv	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
dc.title.translated.eng.fl_str_mv	Geometry and evolution of the Casabe Fault in the Middle Magdalena Valley, Colombia
title	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
spellingShingle	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia 550 - Ciencias de la tierra::551 - Geología, hidrología, meteorología Hundimiento del suelo Falla Casabe Deformación de rumbo Reactivación de fallas Valle Medio del Magdalena Colombia Interpretación sísmica 3D Casabe Fault Strike-slip faults Fault reactivation Middle Magdalena Valley 3D seismic interpretation Deslizamiento de tierra Sismo
title_short	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
title_full	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
title_fullStr	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
title_full_unstemmed	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
title_sort	Geometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, Colombia
dc.creator.fl_str_mv	Vargas Vargas, Mayra Liseth
dc.contributor.advisor.none.fl_str_mv	Galindo Amaya, Pedro Alejandro Camargo Cortés, Guillermo Arturo
dc.contributor.author.none.fl_str_mv	Vargas Vargas, Mayra Liseth
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 Hundimiento del suelo Falla Casabe Deformación de rumbo Reactivación de fallas Valle Medio del Magdalena Colombia Interpretación sísmica 3D Casabe Fault Strike-slip faults Fault reactivation Middle Magdalena Valley 3D seismic interpretation Deslizamiento de tierra Sismo
dc.subject.other.none.fl_str_mv	Hundimiento del suelo
dc.subject.proposal.spa.fl_str_mv	Falla Casabe Deformación de rumbo Reactivación de fallas Valle Medio del Magdalena Colombia Interpretación sísmica 3D
dc.subject.proposal.eng.fl_str_mv	Casabe Fault Strike-slip faults Fault reactivation Middle Magdalena Valley 3D seismic interpretation
dc.subject.unesco.none.fl_str_mv	Deslizamiento de tierra Sismo
description	ilustraciones, graficas, mapas
publishDate	2021
dc.date.issued.none.fl_str_mv	2021
dc.date.accessioned.none.fl_str_mv	2022-02-01T21:45:59Z
dc.date.available.none.fl_str_mv	2022-02-01T21:45:59Z
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	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/80847
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/80847 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
dc.relation.references.spa.fl_str_mv	Acosta, J., Velandia, F., Osorio, J., Lonergan, L., & Mora, H. (2007). Strike-slip deformation within the Colombian Andes. Geological Society Special Publication, 272, 303–319. Bayona, G., Baquero, M., Ramírez, C., Tabares, M., Salazar, A. M., Nova, G., … Cárdenas-Rozo, A. L. (2020). Unravelling the widening of the earliest Andean northern orogen: Maastrichtian to early Eocene intra-basinal deformation in the northern Eastern Cordillera of Colombia. Basin Research, 33(1), 809–845. https://doi.org/10.1111/bre.12496 Bayona, G., Cardona, A., Jaramillo, C., Mora, A., Montes, C., Valencia, V., … IbañezMejia, M. (2012). Early Paleogene magmatism in the northern Andes: Insights on the effects of Oceanic Plateau-continent convergence. Earth and Planetary Science Letters. https://doi.org/10.1016/j.epsl.2012.03.015 Bonini, M., Sani, F., & Antonielli, B. (2012). Basin inversion and contractional reactivation of inherited normal faults: A review based on previous and new experimental models. Tectonophysics, 522–523, 55–88. https://doi.org/10.1016/j.tecto.2011.11.014 Caballero, V. (2010). Evolución tectono - sedimentaria del sinclinal de nuevo mundo, cuenca sedimentaria Valle Medio del Magdalena Colombia, durante el OligocenoMioceno. MSc Thesis Universidad Industrial de Santander. Universidad Industrial de Santander. https://doi.org/10.1128/AAC.03728-14 Caballero, V., Mora, A., Quintero, I., Blanco, V., Parra, M., Rojas, L. E., … Duddy, I. (2013). Tectonic controls on sedimentation in an intermontane hinterland basin adjacent to inversion structures: The Nuevo Mundo syncline, Middle Magdalena Valley, Colombia. Geological Society Special Publication, 377(1), 315–342. https://doi.org/10.1144/SP377.12 Caballero, V., Parra, M., Mora, A., Lopez, C., Rojas, L. E., & Quintero, I. (2013). Factors controlling selective abandonment and reactivation in thick-skin orogens: A case study in the Magdalena Valley, Colombia. Geological Society Special Publication, 377(1), 343–367. https://doi.org/10.1144/SP377.4 Cabello, P., Lopez, C., Gamba, N., Dussán, M. I., Torres, E., Ballesteros-Torres, C. I., … Ramos, E. (2018). An integrated approach to define new plays in mature oil basins: The example from the Middle Magdalena Valley basin (Colombia). AAPG Bulletin, 102(11), 2201–2238. https://doi.org/10.1306/03291816528 Cardona, A., Valencia, V. A., Bayona, G., Duque, J., Ducea, M., Gehrels, G., … Ruiz, J. (2011). Early-subduction-related orogeny in the northern Andes: Turonian to Eocene magmatic and provenance record in the Santa Marta Massif and Rancheria Basin, northern Colombia. Terra Nova. https://doi.org/10.1111/j.1365-3121.2010.00979.x Cetina, L. M., Velandia, F., & Patiño-Sanabria, H. A. (2019). Análisis de deformación al occidente del Anticlinorio de Los Yariguíes - Cordillera Oriental de Colombia. Revista Boletín de Geología, 41(3), 31–56. https://doi.org/10.18273/revbol.v41n3-2019002 Christie-Blick, N., & Biddle, K. T. (1985). Deformation and basin formation along strike-slip faults. In K. T. Biddle & N. Christie-Blick (Eds.), Strike-slip Deformation, Basin Formation, and Sedimentation (pp. 1–34). Tulsa, OK, USA.: Society of Economic Paleontologists and Mineralogists, Special Publication, 37. Cooper, M. A. (1995). Basin development and tectonic history of the Llanos Basin, Eastern Cordillera, and Middle Magdalena Valley, Colombia. American Association of Petroleum Geologists Bulletin, 79(10), 1421–1443. Cooper, M., & Warren, M. J. (2010). The geometric characteristics, genesis and petroleum significance of inversion structures. Geological Society Special Publication, 335, 827– 846. https://doi.org/10.1144/SP335.33 Dooley, T. P., & Schreurs, G. (2012). Analogue modelling of intraplate strike-slip tectonics: A review and new experimental results. Tectonophysics, 574–575, 1–71. https://doi.org/10.1016/j.tecto.2012.05.030 Egbue, O., & Kellogg, J. (2010). Pleistocene to Present North Andean “escape.” Tectonophysics, 489(1–4), 248–257. https://doi.org/10.1016/j.tecto.2010.04.021 Galindo, P. A., & Lonergan, L. (2020). Basin Evolution and Shale Tectonics on an Obliquely Convergent Margin: The Bahia Basin, Offshore Colombian Caribbean. Tectonics, 39(3), 1–32. https://doi.org/10.1029/2019TC005787 Garavito-Cubillos, F. (2008). Structural Analysis of an Area in the Northern Central Part. MSc Thesis Colorado School of Mines. García-Delgado, H., & Velandia, F. (2020). Tectonic geomorphology of the Serranía de San Lucas (Central Cordillera): Regional implications for active tectonics and drainage rearrangement in the Northern Andes. Geomorphology, 349, 106914. https://doi.org/10.1016/j.geomorph.2019.106914 Gómez, E., Jordan, T. E., Allmendinger, R. W., & Cardozo, N. (2005). Development of the Colombian foreland-basin system as a consequence of diachronous exhumation of the northern Andes. Bulletin of the Geological Society of America, 117(9–10), 1272– 1292. https://doi.org/10.1130/B25456.1 Gómez, E., Jordan, T. E., Allmendinger, R. W., Hegarty, K., & Kelley, S. (2005). Syntectonic Cenozoic sedimentation in the northern middle Magdalena Valley Basin of Colombia and implications for exhumation of the Northern Andes. Bulletin of the Geological Society of America, 117(5–6), 547–569. https://doi.org/10.1130/B25454.1 Gómez, E., Jordan, T. E., Allmendinger, R. W., Hegarty, K., Kelley, S., & Heizler, M. (2003). Controls on architecture of the Late Cretaceous to Cenozoic southern Middle Magdalena Valley Basin, Colombia. Bulletin of the Geological Society of America, 115(2), 131–147. https://doi.org/10.1130/0016- 7606(2003)115<0131:COAOTL>2.0.CO;2 Grimaldi, G. O., & Dorobek, S. L. (2011). Fault framework and kinematic evolution of inversion structures: Natural examples from the Neuquén Basin, Argentina. AAPG Bulletin, 95(1), 27–60. https://doi.org/10.1306/06301009165 Horton, B. K., Anderson, V. J., Caballero, V., Saylor, J. E., Nie, J., Parra, M., & Mora, A. (2015). Application of detrital zircon U-Pb geochronology to surface and subsurface correlations of provenance, paleodrainage, and tectonics of the Middle Magdalena Valley Basin of Colombia. Geosphere, 11(6), 1790–1811. https://doi.org/10.1130/GES01251.1 Horton, B. K., Saylor, J. E., Nie, J., Mora, A., Parra, M., Reyes-Harker, A., & Stockli, D. F. (2010). Linking sedimentation in the northern Andes to basement configuration, Mesozoic extension, and Cenozoic shortening: Evidence from detrital zircon U-Pb ages, Eastern Cordillera, Colombia. Bulletin of the Geological Society of America, 122(9–10), 1423–1442. https://doi.org/10.1130/B30118.1 Instituto Colombiano de Geología y Minería INGEMINAS. (2008). Cartografía Geológica y Muestreo Geoquímico escala 1:100.000 de las Planchas 119 Barrancabermeja, 134 Puerto Parra, 149 Puerto Serviez y 150 Cimitarra del Valle Medio del Río Magdalena 11. Retrieved from http://aplicaciones1.sgc.gov.co/sicat/html/ConsultaBasica.aspx Kim, Y.-S., Peacock, D. C. P., & Sanderson, D. J. (2004). Fault damage zones. Journal of Structural Geology, 26(3), 503–517. https://doi.org/10.1016/j.jsg.2003.08.002 Kim, Y. S., Andrews, J. R., & Sanderson, D. J. (2001). Reactivated strike-slip faults: Examples from North Cornwall, UK. Tectonophysics, 340(3–4), 173–194. https://doi.org/10.1016/S0040-1951(01)00146-9 Kim, Y. S., Peacock, D. C. P., & Sanderson, D. J. (2003). Mesoscale strike-slip faults and damage zones at Marsalforn, Gozo Island, Malta. Journal of Structural Geology, 25(5), 793–812. https://doi.org/10.1016/S0191-8141(02)00200-6 MOJICA, J., & FRANCO, R. (1990). Estructura y evolucion tectonica del valle Medio y Superior de Magdalena, Colombia. Geologia Colombiana, 17(17), 41–64 Montes, C., Hatcher, R. D., & Restrepo-Pace, P. A. (2005). Tectonic reconstruction of the northern Andean blocks: Oblique convergence and rotations derived from the kinematics of the Piedras-Girardot area, Colombia. Tectonophysics, 399(1-4 SPEC. ISS.), 221–250. https://doi.org/10.1016/j.tecto.2004.12.024 Montes, C., Rodriguez-Corcho, A. F., Bayona, G., Hoyos, N., Zapata, S., & Cardona, A. (2019). Continental margin response to multiple arc-continent collisions: The northern Andes-Caribbean margin. Earth-Science Reviews. Elsevier. https://doi.org/10.1016/j.earscirev.2019.102903 Mora-Páez, H., Kellogg, J. N., Freymueller, J. T., Mencin, D., Fernandes, R. M. S., Diederix, H., … Bohórquez-orozco, O. (2018). Journal of South American Earth Sciences Crustal deformation in the northern Andes – A new GPS velocity field. Journal of South American Earth Sciences, 89(November 2018), 76–91. https://doi.org/10.1016/j.jsames.2018.11.002 Mora, A., Reyes-Harker, A., Rodriguez, G., Tesón, E., Ramirez-Arias, J. C., Parra, M., … Stockli, D. F. (2013). Inversion tectonics under increasing rates of shortening and sedimentation: Cenozoic example from the Eastern Cordillera of Colombia. Geological Society Special Publication, 377(1), 411–442. https://doi.org/10.1144/SP377.6 Moreno, S., Silva, A., Mora, S., Teso, E., Quintero, I., Rojas, L. E., … Casallas, W. (2013). Interaction between thin- and thick-skinned tectonics in the foothill areas of an inverted graben . The Middle Magdalena Foothill belt, 221–255 Morley, C. K., Gabdi, S., & Seusutthiya, K. (2007). Fault superimposition and linkage resulting from stress changes during rifting: Examples from 3D seismic data, Phitsanulok Basin, Thailand. Journal of Structural Geology, 29(4), 646–663. https://doi.org/10.1016/j.jsg.2006.11.005 Naylor, M. A., Mandl, G., & Supesteijn, C. H. K. (1986). Fault geometries in basementinduced wrench faulting under different initial stress states. Journal of Structural Geology, 8(7), 737–752. https://doi.org/10.1016/0191-8141(86)90022-2 Nie, J., Horton, B. K., Mora, A., Saylor, J. E., Housh, T. B., Rubiano, J., & Naranjo, J. (2010). Tracking exhumation of Andean ranges bounding the Middle Magdalena Valley Basin, Colombia. Geology, 38(5), 451–454. https://doi.org/10.1130/G30775.1 Nie, J., Horton, B. K., Saylor, J. E., Mora, A., Mange, M., Garzione, C. N., … Parra, M. (2012). Integrated provenance analysis of a convergent retroarc foreland system: UPb ages, heavy minerals, Nd isotopes, and sandstone compositions of the Middle Magdalena Valley basin, northern Andes, Colombia. Earth-Science Reviews. https://doi.org/10.1016/j.earscirev.2011.11.002 Peacock, D. C. P., & Sanderson, D. J. (1995). Strike-slip relay ramps. Journal of Structural Geology, 17(10), 1351–1360. https://doi.org/10.1016/0191-8141(95)97303-W Pindell, J. L., & Kennan, L. (2009). Tectonic evolution of the Gulf of Mexico , Caribbean and northern South America in the mantle reference frame: an update. Geological Society, London, Special Publications, 328, 1–55. https://doi.org/10.1144/SP328.1 Reyes-Harker, A., Ruiz-Valdivieso, C. F., Mora, A., Ramírez-Arias, J. C., Rodriguez, G., De La Parra, F., … Blanco, V. (2015). Cenozoic paleogeography of the Andean foreland and retroarc hinterland of Colombia. AAPG Bulletin (Vol. 99). https://doi.org/10.1306/06181411110 Rolon, L. F. (2004). Structural Geometry of the Jura-Cretaceous Rift of the Middle Magdalena Valley Basin – Colombia. MSc Thesis West Virginia University Royero Gutierrez, J. M., & Clavijo, J. (2001). Mapa Geológico Generalizado Departamento de Santander. Sanchez, J., Horton, B. K., Tesón, E., Mora, A., Ketcham, R. A., & Stockli, D. F. (2012). Kinematic evolution of Andean fold-thrust structures along the boundary between the Eastern Cordillera and Middle Magdalena Valley basin, Colombia. Tectonics, 31(3), 1–24. https://doi.org/10.1029/2011TC003089 Sarmiento, G., Puentes, J., & Sierra, C. (2015). Evolución Geológica y Estratigrafía del Sector Norte del Valle Medio del Magdalena, 51–82 Schamel, S. (1991). Middle and Upper Magdalena Basins, Colombia.pdf. AAPG Bulletin. Servicio Geológico Colombiano. (2015). Memoria Expliactiva Plancha 118 - San Francisco. Srisuriyon, K., & Morley, C. K. (2014). Pull-apart development at overlapping fault tips: Oblique rifting of a cenozoic continental margin, northern mergui basin, andaman sea. Geosphere, 10(1), 80–106. https://doi.org/10.1130/GES00926.1 Tchalenko, J. S. (1970). Similarities between Shear Zones of Different Magnitudes. Geological Society of America Bulletin, 81(June), 1625–1640. Velandia, F., Acosta, J., Terraza, R., & Villegas, H. (2005). The current tectonic motion of the Northern Andes along the Algeciras Fault System in SW Colombia. Tectonophysics, 399(1-4 SPEC. ISS.), 313–329. https://doi.org/10.1016/j.tecto.2004.12.028 Velandia, F., & Bermúdez, M. A. (2018). The transpressive southern termination of the Bucaramanga fault (Colombia): Insights from geological mapping, stress tensors, and fractal analysis. Journal of Structural Geology, 115(February), 190–207. https://doi.org/10.1016/j.jsg.2018.07.020
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dc.rights.license.spa.fl_str_mv	Atribución-NoComercial-CompartirIgual 4.0 Internacional
dc.rights.uri.spa.fl_str_mv	http://creativecommons.org/licenses/by-nc-sa/4.0/
dc.rights.accessrights.spa.fl_str_mv	info:eu-repo/semantics/openAccess
rights_invalid_str_mv	Atribución-NoComercial-CompartirIgual 4.0 Internacional http://creativecommons.org/licenses/by-nc-sa/4.0/ http://purl.org/coar/access_right/c_abf2
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dc.format.mimetype.spa.fl_str_mv	application/pdf
dc.coverage.region.none.fl_str_mv	Magdalena Valle Medio del Magdalena
dc.publisher.spa.fl_str_mv	Universidad Nacional de Colombia
dc.publisher.program.spa.fl_str_mv	Bogotá - Ciencias - Maestría en Ciencias - Geología
dc.publisher.department.spa.fl_str_mv	Departamento de Geociencias
dc.publisher.faculty.spa.fl_str_mv	Facultad de Ciencias
dc.publisher.place.spa.fl_str_mv	Bogotá, Colombia
dc.publisher.branch.spa.fl_str_mv	Universidad Nacional de Colombia - Sede Bogotá
institution	Universidad Nacional de Colombia
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spelling	Atribución-NoComercial-CompartirIgual 4.0 Internacionalhttp://creativecommons.org/licenses/by-nc-sa/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Galindo Amaya, Pedro Alejandroedcbc2b5c873aa5d0b30d71b673f1d75Camargo Cortés, Guillermo Arturo49e83b15cf68f7e1cff92a004f535c1aVargas Vargas, Mayra Lisethb99800887d4a7208c80ae78d6a7334cc2022-02-01T21:45:59Z2022-02-01T21:45:59Z2021https://repositorio.unal.edu.co/handle/unal/80847Universidad Nacional de ColombiaRepositorio Institucional Universidad Nacional de Colombiahttps://repositorio.unal.edu.co/ilustraciones, graficas, mapasLa 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)The 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 RecentMaestríaMagíster en Ciencias - GeologíaGeología Estructuralapplication/pdfspaUniversidad Nacional de ColombiaBogotá - Ciencias - Maestría en Ciencias - GeologíaDepartamento de GeocienciasFacultad de CienciasBogotá, ColombiaUniversidad Nacional de Colombia - Sede Bogotá550 - Ciencias de la tierra::551 - Geología, hidrología, meteorologíaHundimiento del sueloFalla CasabeDeformación de rumboReactivación de fallasValle Medio del MagdalenaColombiaInterpretación sísmica 3DCasabe FaultStrike-slip faultsFault reactivationMiddle Magdalena Valley3D seismic interpretationDeslizamiento de tierraSismoGeometría y evolución de la Falla Casabe en el Valle Medio del Magdalena, ColombiaGeometry and evolution of the Casabe Fault in the Middle Magdalena Valley, ColombiaTrabajo de grado - Maestríainfo:eu-repo/semantics/masterThesisinfo:eu-repo/semantics/acceptedVersionTexthttp://purl.org/redcol/resource_type/TMMagdalenaValle Medio del MagdalenaAcosta, J., Velandia, F., Osorio, J., Lonergan, L., & Mora, H. (2007). Strike-slip deformation within the Colombian Andes. Geological Society Special Publication, 272, 303–319.Bayona, G., Baquero, M., Ramírez, C., Tabares, M., Salazar, A. M., Nova, G., … Cárdenas-Rozo, A. L. (2020). Unravelling the widening of the earliest Andean northern orogen: Maastrichtian to early Eocene intra-basinal deformation in the northern Eastern Cordillera of Colombia. Basin Research, 33(1), 809–845. https://doi.org/10.1111/bre.12496Bayona, G., Cardona, A., Jaramillo, C., Mora, A., Montes, C., Valencia, V., … IbañezMejia, M. (2012). Early Paleogene magmatism in the northern Andes: Insights on the effects of Oceanic Plateau-continent convergence. Earth and Planetary Science Letters. https://doi.org/10.1016/j.epsl.2012.03.015Bonini, M., Sani, F., & Antonielli, B. (2012). Basin inversion and contractional reactivation of inherited normal faults: A review based on previous and new experimental models. Tectonophysics, 522–523, 55–88. https://doi.org/10.1016/j.tecto.2011.11.014Caballero, V. (2010). Evolución tectono - sedimentaria del sinclinal de nuevo mundo, cuenca sedimentaria Valle Medio del Magdalena Colombia, durante el OligocenoMioceno. MSc Thesis Universidad Industrial de Santander. Universidad Industrial de Santander. https://doi.org/10.1128/AAC.03728-14Caballero, V., Mora, A., Quintero, I., Blanco, V., Parra, M., Rojas, L. E., … Duddy, I. (2013). Tectonic controls on sedimentation in an intermontane hinterland basin adjacent to inversion structures: The Nuevo Mundo syncline, Middle Magdalena Valley, Colombia. Geological Society Special Publication, 377(1), 315–342. https://doi.org/10.1144/SP377.12Caballero, V., Parra, M., Mora, A., Lopez, C., Rojas, L. E., & Quintero, I. (2013). Factors controlling selective abandonment and reactivation in thick-skin orogens: A case study in the Magdalena Valley, Colombia. Geological Society Special Publication, 377(1), 343–367. https://doi.org/10.1144/SP377.4Cabello, P., Lopez, C., Gamba, N., Dussán, M. I., Torres, E., Ballesteros-Torres, C. I., … Ramos, E. (2018). An integrated approach to define new plays in mature oil basins: The example from the Middle Magdalena Valley basin (Colombia). AAPG Bulletin, 102(11), 2201–2238. https://doi.org/10.1306/03291816528Cardona, A., Valencia, V. A., Bayona, G., Duque, J., Ducea, M., Gehrels, G., … Ruiz, J. (2011). Early-subduction-related orogeny in the northern Andes: Turonian to Eocene magmatic and provenance record in the Santa Marta Massif and Rancheria Basin, northern Colombia. Terra Nova. https://doi.org/10.1111/j.1365-3121.2010.00979.xCetina, L. M., Velandia, F., & Patiño-Sanabria, H. A. (2019). Análisis de deformación al occidente del Anticlinorio de Los Yariguíes - Cordillera Oriental de Colombia. Revista Boletín de Geología, 41(3), 31–56. https://doi.org/10.18273/revbol.v41n3-2019002Christie-Blick, N., & Biddle, K. T. (1985). Deformation and basin formation along strike-slip faults. In K. T. Biddle & N. Christie-Blick (Eds.), Strike-slip Deformation, Basin Formation, and Sedimentation (pp. 1–34). Tulsa, OK, USA.: Society of Economic Paleontologists and Mineralogists, Special Publication, 37.Cooper, M. A. (1995). Basin development and tectonic history of the Llanos Basin, Eastern Cordillera, and Middle Magdalena Valley, Colombia. American Association of Petroleum Geologists Bulletin, 79(10), 1421–1443.Cooper, M., & Warren, M. J. (2010). The geometric characteristics, genesis and petroleum significance of inversion structures. Geological Society Special Publication, 335, 827– 846. https://doi.org/10.1144/SP335.33Dooley, T. P., & Schreurs, G. (2012). Analogue modelling of intraplate strike-slip tectonics: A review and new experimental results. Tectonophysics, 574–575, 1–71. https://doi.org/10.1016/j.tecto.2012.05.030Egbue, O., & Kellogg, J. (2010). Pleistocene to Present North Andean “escape.” Tectonophysics, 489(1–4), 248–257. https://doi.org/10.1016/j.tecto.2010.04.021Galindo, P. A., & Lonergan, L. (2020). Basin Evolution and Shale Tectonics on an Obliquely Convergent Margin: The Bahia Basin, Offshore Colombian Caribbean. Tectonics, 39(3), 1–32. https://doi.org/10.1029/2019TC005787Garavito-Cubillos, F. (2008). Structural Analysis of an Area in the Northern Central Part. MSc Thesis Colorado School of Mines.García-Delgado, H., & Velandia, F. (2020). Tectonic geomorphology of the Serranía de San Lucas (Central Cordillera): Regional implications for active tectonics and drainage rearrangement in the Northern Andes. Geomorphology, 349, 106914. https://doi.org/10.1016/j.geomorph.2019.106914Gómez, E., Jordan, T. E., Allmendinger, R. W., & Cardozo, N. (2005). Development of the Colombian foreland-basin system as a consequence of diachronous exhumation of the northern Andes. Bulletin of the Geological Society of America, 117(9–10), 1272– 1292. https://doi.org/10.1130/B25456.1Gómez, E., Jordan, T. E., Allmendinger, R. W., Hegarty, K., & Kelley, S. (2005). Syntectonic Cenozoic sedimentation in the northern middle Magdalena Valley Basin of Colombia and implications for exhumation of the Northern Andes. Bulletin of the Geological Society of America, 117(5–6), 547–569. https://doi.org/10.1130/B25454.1Gómez, E., Jordan, T. E., Allmendinger, R. W., Hegarty, K., Kelley, S., & Heizler, M. (2003). Controls on architecture of the Late Cretaceous to Cenozoic southern Middle Magdalena Valley Basin, Colombia. Bulletin of the Geological Society of America, 115(2), 131–147. https://doi.org/10.1130/0016- 7606(2003)115<0131:COAOTL>2.0.CO;2Grimaldi, G. O., & Dorobek, S. L. (2011). Fault framework and kinematic evolution of inversion structures: Natural examples from the Neuquén Basin, Argentina. AAPG Bulletin, 95(1), 27–60. https://doi.org/10.1306/06301009165Horton, B. K., Anderson, V. J., Caballero, V., Saylor, J. E., Nie, J., Parra, M., & Mora, A. (2015). Application of detrital zircon U-Pb geochronology to surface and subsurface correlations of provenance, paleodrainage, and tectonics of the Middle Magdalena Valley Basin of Colombia. Geosphere, 11(6), 1790–1811. https://doi.org/10.1130/GES01251.1Horton, B. K., Saylor, J. E., Nie, J., Mora, A., Parra, M., Reyes-Harker, A., & Stockli, D. F. (2010). Linking sedimentation in the northern Andes to basement configuration, Mesozoic extension, and Cenozoic shortening: Evidence from detrital zircon U-Pb ages, Eastern Cordillera, Colombia. Bulletin of the Geological Society of America, 122(9–10), 1423–1442. https://doi.org/10.1130/B30118.1Instituto Colombiano de Geología y Minería INGEMINAS. (2008). Cartografía Geológica y Muestreo Geoquímico escala 1:100.000 de las Planchas 119 Barrancabermeja, 134 Puerto Parra, 149 Puerto Serviez y 150 Cimitarra del Valle Medio del Río Magdalena 11. Retrieved from http://aplicaciones1.sgc.gov.co/sicat/html/ConsultaBasica.aspxKim, Y.-S., Peacock, D. C. P., & Sanderson, D. J. (2004). Fault damage zones. Journal of Structural Geology, 26(3), 503–517. https://doi.org/10.1016/j.jsg.2003.08.002Kim, Y. S., Andrews, J. R., & Sanderson, D. J. (2001). Reactivated strike-slip faults: Examples from North Cornwall, UK. Tectonophysics, 340(3–4), 173–194. https://doi.org/10.1016/S0040-1951(01)00146-9Kim, Y. S., Peacock, D. C. P., & Sanderson, D. J. (2003). Mesoscale strike-slip faults and damage zones at Marsalforn, Gozo Island, Malta. Journal of Structural Geology, 25(5), 793–812. https://doi.org/10.1016/S0191-8141(02)00200-6MOJICA, J., & FRANCO, R. (1990). Estructura y evolucion tectonica del valle Medio y Superior de Magdalena, Colombia. Geologia Colombiana, 17(17), 41–64Montes, C., Hatcher, R. D., & Restrepo-Pace, P. A. (2005). Tectonic reconstruction of the northern Andean blocks: Oblique convergence and rotations derived from the kinematics of the Piedras-Girardot area, Colombia. Tectonophysics, 399(1-4 SPEC. ISS.), 221–250. https://doi.org/10.1016/j.tecto.2004.12.024Montes, C., Rodriguez-Corcho, A. F., Bayona, G., Hoyos, N., Zapata, S., & Cardona, A. (2019). Continental margin response to multiple arc-continent collisions: The northern Andes-Caribbean margin. Earth-Science Reviews. Elsevier. https://doi.org/10.1016/j.earscirev.2019.102903Mora-Páez, H., Kellogg, J. N., Freymueller, J. T., Mencin, D., Fernandes, R. M. S., Diederix, H., … Bohórquez-orozco, O. (2018). Journal of South American Earth Sciences Crustal deformation in the northern Andes – A new GPS velocity field. Journal of South American Earth Sciences, 89(November 2018), 76–91. https://doi.org/10.1016/j.jsames.2018.11.002Mora, A., Reyes-Harker, A., Rodriguez, G., Tesón, E., Ramirez-Arias, J. C., Parra, M., … Stockli, D. F. (2013). Inversion tectonics under increasing rates of shortening and sedimentation: Cenozoic example from the Eastern Cordillera of Colombia. Geological Society Special Publication, 377(1), 411–442. https://doi.org/10.1144/SP377.6Moreno, S., Silva, A., Mora, S., Teso, E., Quintero, I., Rojas, L. E., … Casallas, W. (2013). Interaction between thin- and thick-skinned tectonics in the foothill areas of an inverted graben . The Middle Magdalena Foothill belt, 221–255Morley, C. K., Gabdi, S., & Seusutthiya, K. (2007). Fault superimposition and linkage resulting from stress changes during rifting: Examples from 3D seismic data, Phitsanulok Basin, Thailand. Journal of Structural Geology, 29(4), 646–663. https://doi.org/10.1016/j.jsg.2006.11.005Naylor, M. A., Mandl, G., & Supesteijn, C. H. K. (1986). Fault geometries in basementinduced wrench faulting under different initial stress states. Journal of Structural Geology, 8(7), 737–752. https://doi.org/10.1016/0191-8141(86)90022-2Nie, J., Horton, B. K., Mora, A., Saylor, J. E., Housh, T. B., Rubiano, J., & Naranjo, J. (2010). Tracking exhumation of Andean ranges bounding the Middle Magdalena Valley Basin, Colombia. Geology, 38(5), 451–454. https://doi.org/10.1130/G30775.1Nie, J., Horton, B. K., Saylor, J. E., Mora, A., Mange, M., Garzione, C. N., … Parra, M. (2012). Integrated provenance analysis of a convergent retroarc foreland system: UPb ages, heavy minerals, Nd isotopes, and sandstone compositions of the Middle Magdalena Valley basin, northern Andes, Colombia. Earth-Science Reviews. https://doi.org/10.1016/j.earscirev.2011.11.002Peacock, D. C. P., & Sanderson, D. J. (1995). Strike-slip relay ramps. Journal of Structural Geology, 17(10), 1351–1360. https://doi.org/10.1016/0191-8141(95)97303-WPindell, J. L., & Kennan, L. (2009). Tectonic evolution of the Gulf of Mexico , Caribbean and northern South America in the mantle reference frame: an update. Geological Society, London, Special Publications, 328, 1–55. https://doi.org/10.1144/SP328.1Reyes-Harker, A., Ruiz-Valdivieso, C. F., Mora, A., Ramírez-Arias, J. C., Rodriguez, G., De La Parra, F., … Blanco, V. (2015). Cenozoic paleogeography of the Andean foreland and retroarc hinterland of Colombia. AAPG Bulletin (Vol. 99). https://doi.org/10.1306/06181411110Rolon, L. F. (2004). Structural Geometry of the Jura-Cretaceous Rift of the Middle Magdalena Valley Basin – Colombia. MSc Thesis West Virginia UniversityRoyero Gutierrez, J. M., & Clavijo, J. (2001). Mapa Geológico Generalizado Departamento de Santander.Sanchez, J., Horton, B. K., Tesón, E., Mora, A., Ketcham, R. A., & Stockli, D. F. (2012). Kinematic evolution of Andean fold-thrust structures along the boundary between the Eastern Cordillera and Middle Magdalena Valley basin, Colombia. Tectonics, 31(3), 1–24. https://doi.org/10.1029/2011TC003089Sarmiento, G., Puentes, J., & Sierra, C. (2015). Evolución Geológica y Estratigrafía del Sector Norte del Valle Medio del Magdalena, 51–82Schamel, S. (1991). Middle and Upper Magdalena Basins, Colombia.pdf. AAPG Bulletin.Servicio Geológico Colombiano. (2015). Memoria Expliactiva Plancha 118 - San Francisco.Srisuriyon, K., & Morley, C. K. (2014). Pull-apart development at overlapping fault tips: Oblique rifting of a cenozoic continental margin, northern mergui basin, andaman sea. Geosphere, 10(1), 80–106. https://doi.org/10.1130/GES00926.1Tchalenko, J. S. (1970). Similarities between Shear Zones of Different Magnitudes. Geological Society of America Bulletin, 81(June), 1625–1640.Velandia, F., Acosta, J., Terraza, R., & Villegas, H. (2005). The current tectonic motion of the Northern Andes along the Algeciras Fault System in SW Colombia. Tectonophysics, 399(1-4 SPEC. ISS.), 313–329. https://doi.org/10.1016/j.tecto.2004.12.028Velandia, F., & Bermúdez, M. A. (2018). The transpressive southern termination of the Bucaramanga fault (Colombia): Insights from geological mapping, stress tensors, and fractal analysis. Journal of Structural Geology, 115(February), 190–207. https://doi.org/10.1016/j.jsg.2018.07.020EstudiantesInvestigadoresPúblico generalORIGINAL1098626642.2022 - Mayra Liseth Vargas Vargas.pdf1098626642.2022 - Mayra Liseth Vargas Vargas.pdfTesis de Maestría en Geologíaapplication/pdf8923489https://repositorio.unal.edu.co/bitstream/unal/80847/1/1098626642.2022%20-%20Mayra%20Liseth%20Vargas%20Vargas.pdf67ede4092a35c8359c7617e5401e6d41MD51LICENSElicense.txtlicense.txttext/plain; charset=utf-84074https://repositorio.unal.edu.co/bitstream/unal/80847/2/license.txt8153f7789df02f0a4c9e079953658ab2MD52THUMBNAIL1098626642.2022 - Mayra Liseth Vargas Vargas.pdf.jpg1098626642.2022 - Mayra Liseth Vargas Vargas.pdf.jpgGenerated Thumbnailimage/jpeg4768https://repositorio.unal.edu.co/bitstream/unal/80847/3/1098626642.2022%20-%20Mayra%20Liseth%20Vargas%20Vargas.pdf.jpgb97e46d7e56cb11bda340744b136be64MD53unal/80847oai:repositorio.unal.edu.co:unal/808472023-07-31 23:04:34.303Repositorio Institucional 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EVESURBIFBPUiBMQSBTRUNSRVRBUsONQSBHRU5FUkFMLiAqTEEgVEVTSVMgQSBQVUJMSUNBUiBERUJFIFNFUiBMQSBWRVJTScOTTiBGSU5BTCBBUFJPQkFEQS4gCgpBbCBoYWNlciBjbGljIGVuIGVsIHNpZ3VpZW50ZSBib3TDs24sIHVzdGVkIGluZGljYSBxdWUgZXN0w6EgZGUgYWN1ZXJkbyBjb24gZXN0b3MgdMOpcm1pbm9zLiBTaSB0aWVuZSBhbGd1bmEgZHVkYSBzb2JyZSBsYSBsaWNlbmNpYSwgcG9yIGZhdm9yLCBjb250YWN0ZSBjb24gZWwgYWRtaW5pc3RyYWRvciBkZWwgc2lzdGVtYS4KClVOSVZFUlNJREFEIE5BQ0lPTkFMIERFIENPTE9NQklBIC0gw5psdGltYSBtb2RpZmljYWNpw7NuIDE5LzEwLzIwMjEK

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

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