Procedencia de las areniscas del eoceno temprano (ypresiano) del pozo anh-piedras blancas-1x (cinturón plegado san jacinto) y su relación con la paleogeografía de la margen caribe colombiana

dc.contributorPardo-Trujillo, Andrés
dc.creatorMuñoz Valencia, Jaime Andrés
dc.date2021-07-29T21:14:36Z
dc.date2021-07-29T21:14:36Z
dc.date2021-04-06
dc.date.accessioned2023-09-06T18:27:19Z
dc.date.available2023-09-06T18:27:19Z
dc.identifierhttps://repositorio.ucaldas.edu.co/handle/ucaldas/16936
dc.identifierUniversidad de Caldas
dc.identifierRepositorio institucional Universidad de Caldas
dc.identifierhttps://repositorio.ucaldas.edu.co
dc.identifier.urihttps://repositorioslatinoamericanos.uchile.cl/handle/2250/8697622
dc.descriptionIlustaciones, mapas, fotos
dc.descriptionspa: En el presente trabajo, se presentan los resultados obtenidos a partir del estudio de procedencia de la Formación San Cayetano (Eoceno inferior, Ypresiano) ubicada en la parte norte de la cuenca Cinturón Plegado de San Jacinto. Para ello se estudió el pozo ANH-Piedras Blancas-1X, perforado por la Agencia Nacional de Hidrocarburos en el año 2015. Los nuevos datos incluyen análisis de facies (1038 fotografías), petrografía convencional (102 secciones delgadas), minerales densos (3 secciones), tipología de circones (3 muestras), geocronología U/Pb en circones detríticos de las arenitas (3 muestras), con el fin de determinar las áreas que aportaron sedimentos a la cuenca, la paleogeografía y ambiente sedimentario durante el Eoceno Temprano. La edad del pozo se determinó previamente a partir de la bioestratigrafía de nanofósiles calcáreos obteniendo una edad entre ~53-48.3Ma (Ypresiano). El análisis de facies indica que los sedimentos que conforman estás rocas se depositaron en un sistema de abanico turbidítico. Las areniscas muestran un amplio espectro de composición modal, desde arcosas líticas, litoarenitas feldespáticas y, en menor proporción, arcosas feldespáticas, subarcosas y sublitoarenitas; los diagramas ternarios de procedencia indican campos de orógeno reciclado y arcos transicionales a disectados en una margen tectónicamente activa. Los minerales pesados muestran asociaciones de minerales inestables (9%-15%), tales como hornblenda, clorita, biotita y piroxeno, moderadamente estables como el apatito (6%-8%), estables (2%-16%) como epidota, clinozoisita, zoisita y ultraestables entre 23%-38% (circón, turmalina, rutilos), que permiten interpretar fuentes cercanas, y podrían corresponder a las rocas ígneas y metamórficas descritas en el Valle Inferior del Magdalena. La tipología de circones indica procedencia de granitos de series calco alcalina y calco alcalino rica en K como granodioritas y monzogranitos. Las edades U/Pb en circones detríticos muestran esencialmente dos poblaciones relacionadas al Cretácico (76-84 Ma) con rocas del basamento del Valle Inferior del Magdalena y magmatismo asociado a la cordillera Central (Batolito Antioqueño) y/o Occidental?, y poblaciones de edad Triásica (227-242 Ma), Jurásica (152-185 Ma), y Precámbrica (562-2020 Ma) asociados al basamento ígneo-metamórfico de la Cordillera Central, (e.g. complejos Cajamarca y Puquí) o retrabajamiento de la cobertera sedimentaria. Una pequeña población de circones del Eoceno temprano (52-54 Ma), los cuales sugieren fuentes relacionadas con el VIM, SNSM, o con expresiones volcano-magmáticas, los cuales fueron erosionados y acumulados en la cuenca durante el Paleoceno-Eoceno temprano. Finalmente, con la información obtenida en la presente investigación y para el área de estudio, se propone como principal fuente de aporte de sedimentos las rocas ígneas y metamórficas del basamento del Valle Inferior del Magdalena y, en menor proporción, las unidades del norte de la cordillera Central y rocas asociadas al norte de la cordillera Oriental. A parte de esto se muestra un aporte durante el Eoceno temprano de expresiones magmáticas que pueden estar relacionada con cuerpos plutónicos, tales como el batolito de Santa Marta y el stock de Parashi.
dc.descriptioneng: In the present work, the results obtained from the study of the origin of the San Cayetano Formation (lower Eocene, Ypresiano) located in the northern part of the Cinturón Plegado de San Jacinto basin are presented. For this, the ANH-Piedras Blancas-1X well, drilled by the National Hydrocarbons Agency in 2015, was studied. The new data includes facies analysis (1038 photographs), conventional petrography (102 thin sections), dense minerals (3 sections ), zircon typology (3 samples), U / Pb geochronology in detrital zircons of the arenites (3 samples), in order to determine the areas that contributed sediments to the basin, the paleogeography and sedimentary environment during the Early Eocene. The age of the well was previously determined from the biostratigraphy of calcareous nanofossils, obtaining an age between ~ 53-48.3 Ma (Ypresiano). Facies analysis indicates that the sediments that make up these rocks were deposited in a turbidite fan system. The sandstones show a wide spectrum of modal composition, from lithic arches, feldspathic lithoarenites and, to a lesser extent, feldspathic arches, sub-arches and sublitoarenites; ternary provenance diagrams indicate recycled orogen fields and transitional to dissected arcs in a tectonically active margin. Heavy minerals show unstable mineral associations (9% -15%), such as hornblende, chlorite, biotite and pyroxene, moderately stable as apatite (6% -8%), stable (2% -16%) as epidote, clinozoisite, zoisite and ultrastables between 23% -38% (zircon, tourmaline, rutile), which allow interpreting nearby sources, and could correspond to igneous and metamorphic rocks described in the Lower Magdalena Valley. The typology of zircons indicates the origin of granites from the alkaline calco and alkaline calco series rich in K such as granodiorites and monzogranites. The U / Pb ages in detrital zircons essentially show two populations related to the Cretaceous (76-84 Ma) with rocks from the basement of the Lower Magdalena Valley and magmatism associated with the Central (Antioqueño) and / or Western mountain range? Triassic age (227-242 Ma), Jurassic (152-185 Ma), and Precambrian (562-2020 Ma) associated with the igneous-metamorphic basement of the Central Cordillera, (e.g. Cajamarca and Puquí complexes) or reworking of the sedimentary cover. A small population of zircons from the early Eocene (52-54 Ma), which suggest sources related to the VIM, SNSM, or volcano-magmatic expressions, which were eroded and accumulated in the basin during the Paleocene-early Eocene. Finally, with the information obtained in the present investigation and for the study area, the igneous and metamorphic rocks of the basement of the Lower Magdalena Valley and, to a lesser extent, the northern units of the Central mountain range and associated rocks to the north of the Eastern mountain range. Apart from this, a contribution is shown during the early Eocene of magmatic expressions that may be related to plutonic bodies, such as the Santa Marta batholith and the Parashi stock.
dc.descriptionIntroducción / 2. Objetivos y preguntas a resolver / 3. Localización / 4. Modelos tectónicos del margen nw de sur américa para la cuenca Sinu-San Jacinto / 5. Estratigrafía de la formación San Cayetano (paleocenoecoceno) / 6. Metodología / 7. Resultados / 8. Discusión / 9. Conclusiones / 10. Referencias
dc.descriptionMaestría
dc.descriptionMagister en Ciencias de la Tierra
dc.descriptionPetrografía
dc.formatapplication/pdf
dc.formatapplication/pdf
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dc.languageeng
dc.languagespa
dc.publisherFacultad de Ciencias Exactas y Naturales
dc.publisherManizales
dc.publisherMaestría en Ciencias de la Tierra
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dc.rightsinfo:eu-repo/semantics/closedAccess
dc.subjectCaribe Colombiano
dc.subjectYpresiano
dc.subjectSan Jacinto
dc.subjectSan Cayetano
dc.subjectVIM
dc.subjectCiencias de la tierra
dc.subjectGeología
dc.titleProcedencia de las areniscas del eoceno temprano (ypresiano) del pozo anh-piedras blancas-1x (cinturón plegado san jacinto) y su relación con la paleogeografía de la margen caribe colombiana
dc.typeTrabajo de grado - Maestría
dc.typehttp://purl.org/coar/resource_type/c_bdcc
dc.typeText
dc.typeinfo:eu-repo/semantics/masterThesis
dc.typeinfo:eu-repo/semantics/publishedVersion


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