Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin
The Putumayo Sub-Basin in southwestern Colombia is a significant region for hydrocarbon exploration, supported by its established petroleum systems, including the Villeta Formation, which acts as a source rock, reservoir, and seal. This study examines Interval "A," a limestone interval fro...
- Autores:
-
Alaimo, Maria
- Tipo de recurso:
- Trabajo de grado de pregrado
- Fecha de publicación:
- 2024
- Institución:
- Universidad de los Andes
- Repositorio:
- Séneca: repositorio Uniandes
- Idioma:
- eng
- OAI Identifier:
- oai:repositorio.uniandes.edu.co:1992/75442
- Acceso en línea:
- https://hdl.handle.net/1992/75442
- Palabra clave:
- Hydrocarbon exploration
Putumayo Sub-Basin
Villeta Formation
2D and 3D seismic interpretation
Foreland basin
Geociencias
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- openAccess
- License
- Attribution 4.0 International
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Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| title |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| spellingShingle |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin Hydrocarbon exploration Putumayo Sub-Basin Villeta Formation 2D and 3D seismic interpretation Foreland basin Geociencias |
| title_short |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| title_full |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| title_fullStr |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| title_full_unstemmed |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| title_sort |
Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland Basin |
| dc.creator.fl_str_mv |
Alaimo, Maria |
| dc.contributor.advisor.none.fl_str_mv |
Daroca, Maria Emilie Rossi, Guillermo Nitescu, Bogdan |
| dc.contributor.author.none.fl_str_mv |
Alaimo, Maria |
| dc.contributor.jury.none.fl_str_mv |
Sierra Rojas, Maria Isabel |
| dc.subject.keyword.eng.fl_str_mv |
Hydrocarbon exploration Putumayo Sub-Basin Villeta Formation 2D and 3D seismic interpretation Foreland basin |
| topic |
Hydrocarbon exploration Putumayo Sub-Basin Villeta Formation 2D and 3D seismic interpretation Foreland basin Geociencias |
| dc.subject.themes.spa.fl_str_mv |
Geociencias |
| description |
The Putumayo Sub-Basin in southwestern Colombia is a significant region for hydrocarbon exploration, supported by its established petroleum systems, including the Villeta Formation, which acts as a source rock, reservoir, and seal. This study examines Interval "A," a limestone interval from the Upper Cretaceous of the Villeta Formation. Evaluating its structural framework, accommodation geometry, and hydrocarbon potential through the integration of well data and seismic interpretations from 2D and 3D datasets. Interval "A" comprises three depositional zones characteristic of a foreland basin: the wedge-top, foredeep, and forebulge. The wedge-top is shaped by compressional tectonics, dominated by high-angle reverse faults. The foredeep is controlled by extensional tectonics, characterized by high-angle normal faults, while the forebulge in the easternmost zone exhibits interval thinning and shallow normal faults. Depths for Interval "A" range from -1,220 feet in the foothills to -9,940 feet in the foredeep, with an average of -5,580 feet. Thicknesses range from 16 to 178 feet, averaging approximately 97 feet; with maximum accumulations concentrated in the south-central sub-basin. The hydrocarbon plays in Interval "A" are associated with two main structural domains. In the foothills, faulted anticline traps sealed by reverse faults dominate. However, their reliability is constrained by uncertainties regarding the timing of the completion of their formation relative to the phases of migration during the Miocene. In contrast, within the interior of the foreland basin, closures associated with normal faults predominate, which are temporally aligned with later migration phases. In this context, normal fault closures are considered more reliable exploration targets. |
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2024 |
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2024-11 |
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2025-01-16T15:34:51Z |
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2025-01-16T15:34:51Z |
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Trabajo de grado - Pregrado |
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info:eu-repo/semantics/bachelorThesis |
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eng |
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eng |
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Agencia Nacional de Hidrocarburos (ANH). (2009). Caguán-Putumayo. Informe técnico. Retrieved from https://www.anh.gov.co/documents/2865/Tipo_1_PDF.pdf Agencia Nacional de Hidrocarburos (ANH). (2009). Cartografía geológica de 51,267.45 km² en la cuenca Caguán-Putumayo a partir de sensores remotos a escala 1:100,000 y 739 km² con control de campo a escala 1:50,000 en las planchas IGAC 413 y 414, departamentos de Meta, Caquetá, Putumayo. Universidad Pedagógica y Tecnológica de Colombia. Retrieved from https://www.anh.gov.co/documents/2673/INFORME.pdf Agencia Nacional de Hidrocarburos (ANH). (2010). Caguán-Putumayo: Ronda Colombia 2010 - Tipo 3. Retrieved from https://www.anh.gov.co/es/hidrocarburos/oportunidades-disponibles/procesosde-seleccion/ronda-colombia-2010/tipo-3/cagu%C3%A1n-putumayo/ Allen, P. A., & Allen, J. R. (2005). Basin Analysis: Principles and Applications (2nd ed.). Blackwell Publishing. ISBN 978-0-632-05207-3. (532 p.) Aminzadeh, F., & Dasgupta, S. N. (2013). Fundamentals of petroleum geology. In Developments in Petroleum Science (Vol. 60, p. 15–36). Elsevier. https://doi.org/10.1016/B978-0-444-59599-8.00002-4 Bayona, G., Bustamante, C., Nova, G. & Salazar–Franco, A.M. (2020). Jurassic evolution of the northwestern corner of Gondwana: Present knowledge and future challenges in studying Colombian Jurassic rocks. In: Gómez, J. & Pinilla–Pachon, A.O. (editors), The Geology of Colombia, Volume 2 Mesozoic. Servicio Geológico Colombiano, Publicaciones Geológicas Especiales 36, p. 171–207. Bogotá. https://doi.org/10.32685/pub.esp.36.2019.05 Bjørlykke, K. (Ed.). (2015). Petroleum Geoscience: From Sedimentary Environments to Rock Physics (2nd ed.). Springer. https://doi.org/10.1007/978-3-642-34132-8 Burchette, T. P., & Wright, V. P. (1992). Carbonate ramp depositional systems. Sedimentary Geology, 79(1–4), 3–57. https://doi.org/10.1016/0037-0738(92)90003-A Caineng, Z., Zhi, Y., Zhang, G., Lianhua, H., Rukai, Z., Shizhen, T., Tianfu, W., Shouting, F., Bo, L., Jiangwen, L., Jinxing, D., Yu, C., Hongjun, L., Gang, H., Jun, Y., Huiping, H., Xiaoyu, S., Jiacheng, Z., Rui, Z., ... Na, W. U. (2014). Conventional and unconventional petroleum “orderly accumulation”: Concept and practical significance. Petroleum Exploration and Development, 41(1), 14–30. https://doi.org/10.1016/S1876-3804(14)60003-6 DeCelles, P. G., & Giles, K. A. (1996). Foreland basin systems. Basin Research, 8(2), 105–123. https://doi.org/10.1046/j.1365-2117.1996.01491.x Deming, D. (1994). Overburden rock, temperature, and heat flow. In American Association of Petroleum Geologists eBooks (p. 165–186). https://doi.org/10.1306/m60585c9 Éva Oravecz, Attila Balázs, Taras Gerya, Dave A. May, László Fodor; Competing effects of crustal shortening, thermal inheritance, and surface processes explain subsidence anomalies in inverted rift basins. Geology 2024;; 52 (6): 447–452. doi: https://doi.org/10.1130/G51971.1 Fechi, Y. (2016). Modelo Estructural y Evolutivo del Piedemonte Andino entre Mocoa y Villagarzón, Cuenca del Putumayo, Colombia. Tesis de Maestría. Universidad Nacional de Colombia, 137 p. Ganat, T. a. O. (2020). Prospective resources: Plays, leads, and prospects. In SpringerBriefs in Applied Sciences and Technology (p. 13–19). Springer. https://doi.org/10.1007/978-3-030-45250-6_2 Gonçalves, F. T. T., Mora, C. A., Córdoba, F., Kairuz, E. C., & Giraldo, B. N. (2002). Petroleum generation and migration in the Putumayo Basin, Colombia: Insights from an organic geochemistry and basin modeling study in the foothills. Marine and Petroleum Geology, 19(7), 711–723. https://doi.org/10.1016/S0264-8172(02)00034-X Gonçalves, F. T. T., Mora, C. A., Córdoba, F., Kairuz, E. C., & Giraldo, B. N. (2002). Petroleum generation and migration in the Putumayo Basin, Colombia: Insights from an organic geochemistry and basin modeling study in the foothills. Marine and Petroleum Geology, 19(7), 711–723. https://doi.org/10.1016/S0264-8172(02)00034-X Hallett, D. (2002). Petroleum systems. In Petroleum geology of Libya (pp. 355–416). Elsevier. https://doi.org/10.1016/B978-044450525-5/50010-X Higley, D. K. (2001). The Putumayo-Oriente-Maranon Province of Colombia, Ecuador, and Peru—Mesozoic-Cenozoic and Paleozoic Petroleum Systems (U.S. Geological Survey Digital Data Series 63). U.S. Geological Survey. https://pubs.usgs.gov/dds/dds-063/ James, N. P., & Dalrymple, R. W. (Eds.). (2010). Facies models 4 (4th ed., GEOtext 6, 591 pp.). Geological Association of Canada. Lozano, E., & Zamora, N. (2014). Compilación de la cuenca de Caguán–Putumayo: Tectónica, geociencias básicas (Anexo C). Servicio Geológico Colombiano. Retrieved from https://recordcenter.sgc.gov.co/B20/23008100024725/Documento/Pdf/2105247251103000.pdf Magoon, L. B. (2004). Petroleum system: Natures distribution system for oil and gas. Encyclopedia of Energy, 4, 823–836. https://doi.org/10.1016/B0-12-176480-X/00273-1 Martínez, G. C., Hanson, G., Tariq, H. H., Van der Toorn, J., de Souza, J. A., van der Molen, M., Okprekyi, O., Dandapani, R., & Shah, Z. A. (2021). Chapter 9 - Well-to-seismic tie. In E. Onajite (Ed.), Applied Techniques to Integrated Oil and Gas Reservoir Characterization (pp. 249-271). Elsevier. https://doi.org/10.1016/B978-0-12-817236-0.00009-1 Murcia Leal, L. A. (2002). Reconocimiento geológico del Macizo de Garzón (Publicaciones Geológicas Especiales de Ingeominas No. 24). Bogotá, Colombia: Ministerio de Minas y Energía, Instituto de Investigación e Información Geocientífica Minero-Ambiental y Nuclear; Ingeominas, 55 p. Princeton Dim, C. I., Okonkwo, I. A., Anyiam, O. A., Okeugo, C. G., Maduewesi, C. O., Okeke, K. K., & Umeadi, I. M. (2020). Structural, stratigraphic, and combination traps on outcropping lithostratigraphic units of the Anambra Basin, Southeast Nigeria. Petroleum & Coal, 62(1), 71-83. R., C. G., & Aguilera-B., H. (1980). Geología de la Cuenca del Putumayo. Boletín de Geología, 14(28), 45–71. Retrieved from https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/7137 Rossello, E., Nevistic, V., Salvay, R., Pina, L., & Covellone, G. (2019). Cuenca Putumayo (Colombia). Retrieved from https://www.researchgate.net/publication/337335303_CUENCA_PUTUMAYO_COLOMBIA S&P Global. (2024). Compute the Average Velocity Map. IHS Kingdom Online Help. Retrieved from https://onlinehelp.ihs.com/Energy/Kingdom/TKS_2024/Webhelp/wwhelp/wwhimpl/js/html/wwhelp.htm#href=Tools_menu.100.078.html#1051317 Saeid, E., Bakioglu, K., Kellogg, J., Leier, A., Martinez, J., & Guerrero, E. (2017). Garzón Massif basement tectonics: Structural control on evolution of petroleum systems in upper Magdalena and Putumayo basins, Colombia. Marine and Petroleum Geology, 88, 381–401. https://doi.org/10.1016/j.marpetgeo.2017.08.035 Sahay, V. K. (2009). Efficient mineral and hydrocarbon exploration. National Driller, 30(8), 16–18. SLB. (1998). Oilfield glossary. Retrieved October 26, 2024, from https://glossary.slb.com Van der Toorn, J., Martínez, G. C., Hanson, G., Tariq, H. H., Shalaby, H., van der Molen, M., & Shah, Z. A. (2021). Chapter 7 - Time-to-depth conversion. In E. Onajite (Ed.), Applied Techniques to Integrated Oil and Gas Reservoir Characterization (pp. 213–230). Elsevier. https://doi.org/10.1016/B978-0-12-817236-0.00007-8 Zapata, S., Cardona, A., Jaramillo, C., Valencia, V., & Vervoort, J. (2016). Geoquímica y geocronología U–Pb LA-ICP-MS de unidades volcánicas y plutónicas del jurásico en la región del Putumayo (sur de Colombia): Implicaciones tectónicas y correlaciones regionales. Boletín de Geología, 38(2). https://doi.org/10.18273/revbol.v38n2-2016001 |
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Daroca, Maria EmilieRossi, GuillermoNitescu, Bogdanvirtual::22139-1Alaimo, MariaSierra Rojas, Maria Isabel2025-01-16T15:34:51Z2025-01-16T15:34:51Z2024-11https://hdl.handle.net/1992/75442instname:Universidad de los Andesreponame:Repositorio Institucional Sénecarepourl:https://repositorio.uniandes.edu.co/The Putumayo Sub-Basin in southwestern Colombia is a significant region for hydrocarbon exploration, supported by its established petroleum systems, including the Villeta Formation, which acts as a source rock, reservoir, and seal. This study examines Interval "A," a limestone interval from the Upper Cretaceous of the Villeta Formation. Evaluating its structural framework, accommodation geometry, and hydrocarbon potential through the integration of well data and seismic interpretations from 2D and 3D datasets. Interval "A" comprises three depositional zones characteristic of a foreland basin: the wedge-top, foredeep, and forebulge. The wedge-top is shaped by compressional tectonics, dominated by high-angle reverse faults. The foredeep is controlled by extensional tectonics, characterized by high-angle normal faults, while the forebulge in the easternmost zone exhibits interval thinning and shallow normal faults. Depths for Interval "A" range from -1,220 feet in the foothills to -9,940 feet in the foredeep, with an average of -5,580 feet. Thicknesses range from 16 to 178 feet, averaging approximately 97 feet; with maximum accumulations concentrated in the south-central sub-basin. The hydrocarbon plays in Interval "A" are associated with two main structural domains. In the foothills, faulted anticline traps sealed by reverse faults dominate. However, their reliability is constrained by uncertainties regarding the timing of the completion of their formation relative to the phases of migration during the Miocene. In contrast, within the interior of the foreland basin, closures associated with normal faults predominate, which are temporally aligned with later migration phases. In this context, normal fault closures are considered more reliable exploration targets.La subcuenca Putumayo, ubicada en el suroeste de Colombia, es una región fundamental para la exploración de hidrocarburos, respaldada por sistemas petroleros establecidos, incluida la Formación Villeta; que cumple funciones de roca generadora, reservorio y sello. Este estudio se centra en el análisis del Intervalo "A", un intervalo de caliza del Cretácico Superior dentro de la Formación Villeta. Evaluando su marco estructural, geometría de acomodación y potencial de hidrocarburos mediante la integración de datos de pozos y la interpretación de datos sísmicos 2D y 3D. El Intervalo "A" comprende las tres zonas deposicionales características de una cuenca de antepaís: el wedge-top, el foredeep y el forebulge. El wedge-top está influenciado por tectónica compresional y dominado por fallas inversas de alto ángulo. El foredeep está controlado por tectónica extensional, caracterizada por fallas normales de alto ángulo, mientras que el forebulge, ubicado en la zona más oriental, presenta adelgazamiento del intervalo y fallas normales someras. Las profundidades del Intervalo "A" oscilan entre -1220 pies en el piedemonte y -9940 pies en el foredeep, con un promedio de -5580 pies. Los espesores varían entre 16 y 178 pies, con un promedio aproximado de 97 pies, y las acumulaciones máximas se concentran en la subcuenca centro-sur. Los plays de hidrocarburos en el Intervalo "A" están asociados a dos dominios estructurales principales. En el piedemonte predominan las trampas de anticlinales fallados selladas por fallas inversas. Sin embargo, su confiabilidad está condicionada por las incertidumbres en la cronología de finalización de formación de su geometría en relación con las fases de migración ocurridas durante el Mioceno. Por otro lado, hacia el interior de la cuenca de antepaís, predominan los cierres asociados a fallas normales, que se alinean temporalmente con las fases de migración posteriores. En este contexto, los cierres por fallas normales se presentan como objetivos de exploración más confiables. Se resalta la interacción entre los regímenes tectónicos compresionales y extensionales en la configuración de diversos mecanismos de entrampamiento asociados al Intervalo "A". Los resultados ofrecen un panorama para optimizar las estrategias de exploración y respaldar el desarrollo energético en Colombia.Pregrado54 páginasapplication/pdfengUniversidad de los AndesGeocienciasFacultad de CienciasDepartamento de GeocienciasAttribution 4.0 Internationalhttp://creativecommons.org/licenses/by/4.0/info:eu-repo/semantics/openAccesshttp://purl.org/coar/access_right/c_abf2Hydrocarbon prospectivity within the interval “A” of the Villeta Formation in the Putumayo Foreland BasinTrabajo de grado - Pregradoinfo:eu-repo/semantics/bachelorThesisinfo:eu-repo/semantics/acceptedVersionhttp://purl.org/coar/resource_type/c_7a1fTexthttp://purl.org/redcol/resource_type/TPHydrocarbon explorationPutumayo Sub-BasinVilleta Formation2D and 3D seismic interpretationForeland basinGeocienciasAgencia Nacional de Hidrocarburos (ANH). (2009). Caguán-Putumayo. Informe técnico. Retrieved from https://www.anh.gov.co/documents/2865/Tipo_1_PDF.pdfAgencia Nacional de Hidrocarburos (ANH). (2009). Cartografía geológica de 51,267.45 km² en la cuenca Caguán-Putumayo a partir de sensores remotos a escala 1:100,000 y 739 km² con control de campo a escala 1:50,000 en las planchas IGAC 413 y 414, departamentos de Meta, Caquetá, Putumayo. Universidad Pedagógica y Tecnológica de Colombia. Retrieved from https://www.anh.gov.co/documents/2673/INFORME.pdfAgencia Nacional de Hidrocarburos (ANH). (2010). Caguán-Putumayo: Ronda Colombia 2010 - Tipo 3. Retrieved from https://www.anh.gov.co/es/hidrocarburos/oportunidades-disponibles/procesosde-seleccion/ronda-colombia-2010/tipo-3/cagu%C3%A1n-putumayo/Allen, P. A., & Allen, J. R. (2005). Basin Analysis: Principles and Applications (2nd ed.). Blackwell Publishing. ISBN 978-0-632-05207-3. (532 p.)Aminzadeh, F., & Dasgupta, S. N. (2013). Fundamentals of petroleum geology. In Developments in Petroleum Science (Vol. 60, p. 15–36). Elsevier. https://doi.org/10.1016/B978-0-444-59599-8.00002-4Bayona, G., Bustamante, C., Nova, G. & Salazar–Franco, A.M. (2020). Jurassic evolution of the northwestern corner of Gondwana: Present knowledge and future challenges in studying Colombian Jurassic rocks. In: Gómez, J. & Pinilla–Pachon, A.O. (editors), The Geology of Colombia, Volume 2 Mesozoic. Servicio Geológico Colombiano, Publicaciones Geológicas Especiales 36, p. 171–207. Bogotá. https://doi.org/10.32685/pub.esp.36.2019.05Bjørlykke, K. (Ed.). (2015). Petroleum Geoscience: From Sedimentary Environments to Rock Physics (2nd ed.). Springer. https://doi.org/10.1007/978-3-642-34132-8Burchette, T. P., & Wright, V. P. (1992). Carbonate ramp depositional systems. Sedimentary Geology, 79(1–4), 3–57. https://doi.org/10.1016/0037-0738(92)90003-ACaineng, Z., Zhi, Y., Zhang, G., Lianhua, H., Rukai, Z., Shizhen, T., Tianfu, W., Shouting, F., Bo, L., Jiangwen, L., Jinxing, D., Yu, C., Hongjun, L., Gang, H., Jun, Y., Huiping, H., Xiaoyu, S., Jiacheng, Z., Rui, Z., ... Na, W. U. (2014). 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Chapter 7 - Time-to-depth conversion. In E. Onajite (Ed.), Applied Techniques to Integrated Oil and Gas Reservoir Characterization (pp. 213–230). Elsevier. https://doi.org/10.1016/B978-0-12-817236-0.00007-8Zapata, S., Cardona, A., Jaramillo, C., Valencia, V., & Vervoort, J. (2016). Geoquímica y geocronología U–Pb LA-ICP-MS de unidades volcánicas y plutónicas del jurásico en la región del Putumayo (sur de Colombia): Implicaciones tectónicas y correlaciones regionales. 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