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dc.contributor.advisorMarin Arias, Juan Pablo
dc.contributor.authorJaramillo Molina, Manuel
dc.contributor.authorRestrepo Ruiz, Nicolas
dc.contributor.authorRivera Castaño, Andres
dc.date.accessioned2022-01-19T22:15:25Z
dc.date.available2022-01-19T22:15:25Z
dc.date.issued2022-01-20
dc.identifier.urihttps://repositorio.ucaldas.edu.co/handle/ucaldas/17354
dc.descriptionIlustraciones, mapas, gráficasspa
dc.description.abstractspa: Esta tesis está desarrollada en la zona noroeste de la cuenca del Golfo de México en el área de Matagorda Island, Estados Unidos. La cuenca del Golfo de México es una de las más estudiadas y prospectivas en el mundo. Este trabajo identifica y analiza un prospecto con alta probabilidad de contener hidrocarburos para ser explotado. El estudio se basó en la siguiente metodología: recopilación bibliográfica, extrapolación de información bioestratigráfica, interpretación sísmica y petrofísica, identificación de leads y prospecto. Este proceso llevó a la identificación del prospecto Rango; analizado por medio de registros de pozos, información bioestratigráfica y mapas de contornos creados a partir de la sísmica. El prospecto está ubicado en el Mioceno Inferior marcado por el microfósil Robulus L-43 a una profundidad aproximada de 2353 m. La estructura de trampa corresponde a un anticlinal roll-over formado por una falla lístrica y cortado por una falla normal antitética. Se estima una porosidad del 25% para el reservorio con buenas características de permeabilidad. Se observan en los registros altos espesores de shale, creando un sello óptimo. Adicionalmente, para este proyecto, se analizó la posibilidad de reducir las emisiones de CO_2 mediante la captura y almacenamiento del CO_2, inyectándolo en un acuífero salino en la zona estudiada. Se concluye que el prospecto Rango, en el P50, presenta un área de 859 acres con 134 BCF de reservas de gas, almacenadas en una estructura con cierre en cuatro direcciones en la parte superior y tres direcciones contra la falla normal, en la parte inferior. La probabilidad de éxito para el prospecto se estimó en 46% basándose en los elementos del sistema petrolífero: roca fuente (presencia, madurez y migración), roca reservorio, roca sello y trampa.spa
dc.description.abstracteng: This tesis is developed in northwestern section of the Gulf of Mexico Basin in the Matagorda Island area, United States. The Gulf of Mexico Basin is one of the most studied and prospective sedimentary basins in the world. This work identifies and studies a prospect with high probabilities of containing hydrocarbon reserves that can be produced. The study was based on the following methodology: bibliography gathering, extrapolation of biostratigraphic information, seismic and petrophyisical interpretation, leads identification, and prospect evaluation. This process led to the identification of the prospect named Rango, which was analyzed through well logs, biostratigraphic data, and contour maps created from the seismic. The prospect is in the Lower Miocene rocks marked by the microfossil Robulus L-43 at a depth of 2353m. The trap structure is made by a rollover anticline formed by a listric fault and is cut by a normal antithetic fault. A 25% porosity and good permeability is estimated for the reservoir. The well logs display thick beds of shale making up a great seal. Furthermore, this project considers a plan to reduce the CO2 emissions through the carbon capture and storage technology by injecting the produced CO2 in a saline aquifer in the area of interest. To conclude, the Rango prospect, in its P50, presents an area of 859 acres with 134 BCF of gas reserves contained in a four-way closure trap in the upper part, and a three-way closure and a normal fault in the lower part. The probability of success for this prospect was estimated at 46% based on the elements of the petroleum system: source rock, reservoir rock, seal rock, and trap.eng
dc.description.tableofcontents1. Introducción/1 2. Objetivos / 2.1 Objetivo general/ 2.2 Objetivos específicos / 3. Metodología/ 4. Datos e información utilizada/ 4.1 sísmica 3d / 4.2 pozos/ 4.3 carta bioestratigráfica / 5. antecedentes / 6. marco teórico/ 6.1 registros eléctricos / 6.1.1 registro de gamma ray / 6.1.2 registro de potencial espontáneo (sp)/ 6.1.3 registro de resistividad / 6.1.4 registro sónico / 6.1.5 registro de resistividad de agua (𝑅��������������������������������������������������������������������������������𝑤��������������������������������������������������������������������������������𝑎��������������������������������������������������������������������������������)/ 6.1.6 checkshot/ 6.2 método sísmico / 6.3 software opendtect/ 6.4 interpretación sísmica / 6.5 tipos de datos sísmicos: 2d, 3d y 4d/ 6.6 herramientas básicas de interpretación/ 6.6.1 trazado automático, manual y creación de superficies/ 6.6.2 herramienta de visualización 2d y 3d / 6.6.3 herramienta de trazado de fallas/ 6.6.4 herramienta de atributos/ 6.7 acuerdo de parís y cambio climático / 6.8 métodos de captura de carbono / 6.8.1 captura precombustión / 6.8.2 captura postcombustión/ 6.8.3 captura por combustión oxy-fuel/ 6.9 transporte de dióxido de carbono / 6.9.1 tubería / 6.10 almacenamiento de carbono / 6.10.1 almacenamiento en campos de petróleo y gas abandonados/ 6.10.2 almacenamiento en acuíferos salinos profundos / 6.11 incentivos de reducción de impuestos / 7. marco geológico regional / 7.1 marco tectónico/7.1.1 formación del Golfo de México / 7.2 estratigrafía y prospectividad de la cuenca Matagorda islam / 7.2.1 ambiente de depositación / 7.2.2 sistema petrolífero – noroeste golfo de México / 8. análisis y procesamiento de información / 8.1 interpretación petrofísica/ 8.2 determinación de la porosidad/ 8.3 cálculo de la saturación de hidrocarburos./ 8.4 mapeo e interpretación sísmica/ 8.5 identificación de leads / 9. resultados/ 9.1 prospecto rango/ 9.2 correlación petrofísica/ 9.3 estimación de reservas / 9.3.1 factor de corrección geométrica (gf) / 9.3.2 factor de corrección volumétrica para gas (bg): / 9.4 conversión tiempo profundidad – función de velocidad/ 9.5 análisis de riesgo/ 9.5.1 roca fuente y carga de hidrocarburos/ 9.5.2 roca reservorio / 9.5.3 trampa/ 9.5.4 roca sello/ 9.6 propuesta de captura de carbono/ 9.6.1 tecnología de captura de carbono postcombustión/ 9.6.2 transporte del co2 / 9.6.3 almacenamiento de co2 en el área de Matagorda islan/ 9.6.4 monitoreo del co2 inyectado/ 9.6.5 costo de captura y almacenamiento de co2 / 10. Discusión / 11. Conclusiones / 12. Referencias.spa
dc.format.mimetypeapplication/pdfspa
dc.language.isoengspa
dc.language.isospaspa
dc.titleAnálisis de prospectividad de hidrocarburos en la zona de Matagorda islan en la cuenca del golfo de México, Estados unidosspa
dc.typeTrabajo de grado - Pregradospa
dc.contributor.researchgroupGeología (Categoría C)spa
dc.description.degreelevelUniversitariospa
dc.identifier.instnameUniversidad de Caldasspa
dc.identifier.reponameRepositorio institucional Universidad de Caldasspa
dc.identifier.repourlhttps://repositorio.ucaldas.edu.co/spa
dc.publisher.facultyFacultad de Ciencias Exactas y Naturalesspa
dc.publisher.placeManizalesspa
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dc.subject.lembHidrocarburos
dc.subject.lembEstratigrafía
dc.subject.lembPetrografía
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