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Procesos de silicificación de las unidades del Turoniano – Campaniano en la Cuenca Cretácica Colombiana
dc.rights.license | Atribución-NoComercial-SinDerivadas 4.0 Internacional |
dc.contributor.advisor | Sarmiento Pérez, Gustavo Adolfo |
dc.contributor.advisor | Bonilla Osorio, German Eduardo |
dc.contributor.author | Herrera Quijano, Sergio |
dc.date.accessioned | 2021-06-16T15:48:56Z |
dc.date.available | 2021-06-16T15:48:56Z |
dc.date.issued | 2020 |
dc.identifier.uri | https://repositorio.unal.edu.co/handle/unal/79638 |
dc.description | ilustraciones, fotografías, mapas |
dc.description.abstract | La silicificación, en el registro litológico del Cretácico superior colombiano se encuentra presente en ciertas unidades litoestratigráficas de las cuencas sedimentarias del valle del río Magdalena y la cordillera oriental, tales como, las formaciones Lidita Superior, Lidita Inferior, Plaeners, Frontera y la Luna. De estas, se tomaron muestras en los niveles con silicificación y posteriormente se analizaron con técnicas petrográficas (microscopia óptica, cátodoluminiscencia y microscopia electrónica de barrido) y litogeoquímicas (difracción de rayos X, fluorescencia de rayos X y espectrometría de energía dispersiva) que permitieron caracterizar sus propiedades geoquímicas y texturales. Para clasificar más asertivamente las muestras recolectadas, se planteó un cuadro que relaciona sus características texturales con su porcentaje de sílice que, a la vez, se vincula directamente con el grado de silicificación. A partir de esta clasificación, las observaciones y los datos adquiridos, se determinó que los cherts enmarcados dentro del contexto sedimentario calcáreo somero del Cretácico colombiano, se originaron inmediatamente posterior al depósito del sedimento, bajo un mecanismo diagenético temprano que incluye la interacción de la materia orgánica con las bacterias aeróbicas y anaeróbicas, las cuales, modifican las condiciones termodinámicas de equilibrio en los primeros metros del sedimento facilitando la precipitación de polimorfos de sílice. En ese orden de ideas, se plantea que la fuente más probable de la sílice precipitada en estas rocas es proveniente del medio marino, en donde los polímeros e iones de silicio disueltos, aprovechan la permeabilidad sedimentaria y logran llegar a las zonas microbiales con condiciones geoquímicas idóneas para la nucleación de sílice, y de esta manera, cementar y remplazar los componentes originales del sedimento. |
dc.description.abstract | Silicification, in the lithological record of the Colombian Upper Cretaceous, is present in certain lithostratigraphic units of the sedimentary basins of the Magdalena river valley and the eastern mountain range, such as the Lidita Superior, Lidita Inferior, Plaeners, Frontera and La Luna formations. From these, samples were taken at the levels with silicification and subsequently analyzed with petrographic techniques (optical microscopy, cathodoluminescence and scanning electron microscopy) and lithogeochemicals (X-ray diffraction, X-ray fluorescence and energy dispersive spectrometry) that allowed to characterize its geochemical and textural properties. To classify the collected samples more assertively, a table was proposed that relates their textural characteristics with their silica percentage, which, in turn, is directly linked to the degree of silicification. From this classification, the observations and the data acquired, it was determined that the cherts framed within the shallow calcareous sedimentary context of the Colombian Cretaceous, originated immediately after the deposit of the sediment, under an early diagenetic mechanism that includes the interaction of organic matter with aerobic and anaerobic bacteria, which modify the thermodynamic conditions of equilibrium in the first few meters of the sediment, facilitating the precipitation of silica polymorphs. In this vein, it is suggested that the most likely source of precipitated silica in these rocks is from the marine environment, where dissolved silicon polymers and ions take advantage of the sedimentary permeability and reach microbial areas with ideal geochemical conditions for the nucleation of silica, and in this way, cement and replace the original components of the sediment. |
dc.format.extent | 1 recurso en linea (193 paginas) |
dc.format.mimetype | application/pdf |
dc.language.iso | spa |
dc.publisher | Universidad Nacional de Colombia |
dc.rights | Derechos Reservados - Universidad Nacional de Colombia, 2021 |
dc.rights.uri | http://creativecommons.org/licenses/by-nc-nd/4.0/ |
dc.subject.ddc | 558 - Ciencias de la tierra de América del Sur |
dc.title | Procesos de silicificación de las unidades del Turoniano – Campaniano en la Cuenca Cretácica Colombiana |
dc.type | Trabajo de grado - Maestría |
dc.type.driver | info:eu-repo/semantics/masterThesis |
dc.type.version | info:eu-repo/semantics/acceptedVersion |
dc.publisher.program | Bogotá - Ciencias - Maestría en Ciencias - Geología |
dc.contributor.researchgroup | LATTICE |
dc.coverage.country | Colombia |
dc.description.degreelevel | Maestría |
dc.description.degreename | Magíster en Ciencias - Geología |
dc.description.researcharea | Diagénesis |
dc.identifier.instname | Universidad Nacional de Colombia |
dc.identifier.reponame | Repositorio Institucional Universidad Nacional de Colombia |
dc.identifier.repourl | https://repositorio.unal.edu.co/ |
dc.publisher.department | Departamento de Geociencias |
dc.publisher.faculty | Facultad de Ciencias |
dc.publisher.place | Bogotá, Colombia |
dc.publisher.branch | Universidad Nacional de Colombia - Sede Bogotá |
dc.relation.references | Arthur, M. A., Schlanger, S. O., y Jenkyns, H. C. (1987). The Cenomanian-Turonian Oceanic Anoxic Event, II. Palaeoceanographic controls on organicmatter production and preservation. Geological Society Special Publication,26, 401–420. https://doi.org/10.1144/GSL.SP.1987.026.01.25 |
dc.relation.references | Aspden, J. A. (1984). Geología de la Cordillera Occidental y la Costa Pacífica del Departamento del Valle del Cauca, Planchas 261 - 278 - 279 - 280 - 299. |
dc.relation.references | Balthasar, U., y Cusack, M. (2015). Aragonite-calcite seas-Quantifying the gray area. Geology, 43(2), 99–102. https://doi.org/10.1130/G36293.1 |
dc.relation.references | Barrero, D., Pardo, A., Vargas, C. A., y Martínez, J. F. (2007). Colombian Sedimentary Basins: Nomenclature, boundaries and Petroleum Geology, a New Proposal. En Agencia Nacional de Hidrocarburos (ANH) y B&M Exploration Ltda (Eds.), Agencia Nacional de Hidrocarburos - A.N.H.- (Issues 978-958-98237-0–5). https://doi.org/ISBN: 978-958-98237-0-5 |
dc.relation.references | Bathurst, R. G. C. (1966). Boring algae, micrite envelopes and lithification of molluscan biosparites. Geological Journal, 5(1), 15–32. https://doi.org/10.1002/gj.3350050104 |
dc.relation.references | Bayona, G., Cortés, M., Jaramillo, C., Ojeda, G., Aristizabal, J. J., y Reyes-Harker,A. (2008). An integrated analysis of an orogen-sedimentary basin pair: Latest Cretaceous-Cenozoic evolution of the linked Eastern Cordillera orogen and the Llanos foreland basin of Colombia. Bulletin of the Geological Society of America, 120(9–10), 1171–1197. https://doi.org/10.1130/B26187.1 |
dc.relation.references | Boggs, S. (2006). Principles of Sedimentology and stratigraphy (P. Lynch, S. Hale, y G. Dulles (eds.); 4th ed.). Pearson Prentice Hall. https://doi.org/10.1017/CBO9781107415324.004 |
dc.relation.references | Bonilla, G. E., Sarmiento Pérez, G. A., y Gaviria Melo, S. (2011). Proveniencia y transformación diagenética de minerales arcillosos del Maastrichtiano - Paleoceno al norte de Bogotá , Cordillera Oriental de Colombia. Geología Colombiana., 36(1), 179–195. |
dc.relation.references | Bramlette, M. N. (1946). The Monterrey Formation of California and Origin of its Siliceus Rocks. En Professional Paper 212. |
dc.relation.references | Branquet, Y., Cheilletz, A., Cobbold, P. R., Baby, P., Laumonier, B., y Giuliani, G. (2002). Andean deformation and rift inversion, eastern edge of Cordillera Oriental (Guateque-Medina area), Colombia. Journal of South American Earth Sciences, 15(4), 391–407. https://doi.org/10.1016/S0895-9811(02)00063-9 |
dc.relation.references | Briggs, D. E. G., Raiswell, R., Bottrell, S. H., Hatfield, D., y Bartels, C. (1996). Controls on the pyritization of exceptionally preserved fossils: An analysis of the Lower Devonian Hunsrück Slate of Germany. American Journal of Science, 296(6), 633–663. https://doi.org/10.2475/ajs.296.6.633 |
dc.relation.references | Bürgl, H. (1961a). Geología de los alrededores de Ortega, Tolima. Boletín de Geología, 8, 21–38. https://doi.org/10.18273 |
dc.relation.references | Bürgl, H. (1961b). Historia Geologica De Colombia. Revista de La Academia Colombiana de Ciencias, XI(43), 137–191. |
dc.relation.references | Bürgl, H., y Dumit Tobon, Y. (1954). El Cretaceo Superior en la Region de Giradot. Boletín Geológico, II(1), 23–48. |
dc.relation.references | Bustillo, M. A. (2001). Cherts with Moganite in Continental Mg-Clay Deposits: An Example of “False” Magadi-Type Cherts, Madrid Basin, Spain. Journal of Sedimentary Research, 71(3), 436–443. https://doi.org/10.1306/2DC40953-0E47-11D7-8643000102C1865D |
dc.relation.references | Bustillo, M. A., Elorza, J., y Díez-Canseco, D. (2017). Silicificaciones selectivas en Thalassinoides y otras estructuras biogénicas asociadas a calizas de plataforma marina y hardground (Albiense inferior, Sonabia, Cantabria). Estudios Geologicos, 73(1),1–19. https://doi.org/10.3989/egeol.42668.435 |
dc.relation.references | Cáceres, C., y Etayo Serna, F. (1969). Bosquejo Geológico de la Región del Tequendama. En 1er Congreso Colombiano de Geología, Opúsculo guía, Excursión pre–congreso. [s.n.]. |
dc.relation.references | Carson, G. A. (1987). Silicification fabrics from the Cenomanian and basal Turonian of Devon, England: isotopic results. Geological Society, London, Special Publications, 36(1), 87–102. https://doi.org/10.1144/GSL.SP.1987.036.01.08 |
dc.relation.references | Cecil, C. B. (2015). Paleoclimate and the origin of Paleozoic chert: time to reexamine the origins of chert in the rock record. The Sedimentary Record, 13(3), 4–10. https://www.researchgate.net/profile/C_Cecil/publication/281404996_Paleoclimate_and_the_origin_of_Paleozoic_chert_Time_to_reexamine_the_origin_of_chert_in_the_rock_record/links/55e72acd08ae21d099c148d2.pdf |
dc.relation.references | Cediel, F. (1968). El Grupo Giron: Una Molasa Mesozoica de la Cordillera Oriental. Boletin Geolgico, XVI(1–3), 5–96. |
dc.relation.references | Choquette, P. ., y Pray, L. . (1970). Geologic Nomenclature and Classification of Porosity in Sedimentary Carbonates. American Association of Petroleum Geologists Bulletin, 54(2), 207–250. https://doi.org/10.1306/5d25c98b-16c1-11d7-8645000102c1865d |
dc.relation.references | Clavijo, J. (1995). Mapa Geológico De Colombia Plancha 75 - Aguachica. |
dc.relation.references | Cook, P. J., y Shergold, J. H. (1986). Proterozoic and Cambrian phosphorites - an introduction. Phosphate Deposits of the World, Vol. 1: Proterozoic and Cambrian Phosphorites, 1, 1–8. |
dc.relation.references | Corrigan, H. T. (1967). Guidebook to the geology of the upper Magdalena basin, northern portion. Colombian Society of Petroleum Geologists and Geophysists. |
dc.relation.references | De Porta, J. (1965). La Estratigrafía del Cretácico Superior y Terciario en el Extremo S del Valle Medio del Magdalena. Boletín De Geología, 19(1), 5–50. https://doi.org/10.18273/revbol |
dc.relation.references | DeMaster, D. J. (2003). The Diagenesis of Biogenic Silica: Chemical Transformations Occurring in the Water Column, Seabed, and Crust. En Treatise on Geochemistry (Vol. 1, Issue 4, pp. 87–98). Elsevier. https://doi.org/10.1016/B0-08-043751-6/07095-X |
dc.relation.references | Dunham, R. J. (1962). Classification of Carbonate Rocks According to Depositional Texture. Classification of Carbonate Rocks: American Association of Petroleum Geologists Memoir, 108–121. http://archives.datapages.com/data/specpubs/carbona2/data/a038/a038/0001/0100/0108.htm |
dc.relation.references | Etayo Serna, F. (1968). El Sistema Cretáceo en la Región de Villa de Leiva y Zonas Próximas. Geología Colombiana, 5(0), 5–74. |
dc.relation.references | Etayo Serna, F. (1994). Estudios geológicos del Valle Superior del Magdalena. Universidad Nacional de Colombia, Departamento de Geociencias. |
dc.relation.references | Etayo Serna, F., Renzoni, G., y Barrero, D. (1969). Contornos Sucesivos del Mar Cretáceo en Colombia. En F. Etayo-Serna y C. Caceres-Giron (Eds.), Primer Congreso Colombiano de Geología (pp. 217–252). Universidad Nacional de Colombia. |
dc.relation.references | Folk, R. L. (1980). Petrology of Sedimentary Rocks. Hemphill Publishing Company. |
dc.relation.references | Fuquen, J. A., Nuñez Tello, A., y Acosta, J. E. (1993). Geología de la Plancha 282 “Chaparral - Tolima”, Colombia. |
dc.relation.references | Gao, G; Land, L. S. (1991). Nodular chert from the Arbuckle Group, Slick Hills, SW Oklahoma: a combined field, petrographic and isotopic study. Sedimentology, 857–870. |
dc.relation.references | Guan, C., Wang, W., Zhou, C., Muscente, A. D., Wan, B., Chen, X., Yuan, X., Chen, Z., y Ouyang, Q. (2017). Controls on fossil pyritization: Redox conditions, sedimentary organic matter content, and Chuaria preservation in the Ediacaran Lantian Biota. Palaeogeography, Palaeoclimatology, Palaeoecology, 474, 26–35. https://doi.org/10.1016/j.palaeo.2016.05.013 |
dc.relation.references | Guerrero, J., Sarmiento, G., y Navarrete, R. (2000). The Stratigraphy of the W Side of the Cretaceous Colombian Basin in the Upper Magdalena Valley. Reevaluation of Selected Areas and Type Localities Including Aipe, Guaduas, Ortega, and Piedras. Geología Colombiana, 25, 45–110. |
dc.relation.references | Hardie, L. A. (1996). Secular variation in seawater chemistry: An explanation for the coupled secular variation in the mineralogies of marine limestones and 164 Procesos de Silicificación de las Unidades del Turoniano – Campaniano en la Cuenca Cretácica Colombiana potash evaporites over the past 600 m.y. Geology, 24(3), 279–283. https://doi.org/10.1130/0091-7613(1996)024<0279:SVISCA>2.3.CO;2 |
dc.relation.references | Harrison, W. E., Hesse, R., y Gieskes, J. M. (1982). Relationship between Sedimentary Facies and Interstitial Water Chemistry of Slope, Trench, and Cocos Plate Sites from the Middle America Trench Transect, Active Margin off Guatemala, Deep Sea Drilling Project Leg 67. En Initial Reports of the Deep Sea Drilling Project, 67 (Vol. 498, Issue October 2013, pp. 1–224). U.S. Government Printing Office. https://doi.org/10.2973/dsdp.proc.67.129.1982 |
dc.relation.references | Heath, G. R., y Moberly, R. (1971). Cherts from the Western Pacific, Leg.7, DSDP. Initial Reports of the Deep Sea Drilling Project, 7, 991–1007. https://doi.org/10.1126/science.166.3910.1311 |
dc.relation.references | Hernández, S. (2020). Litogeoquímica de las Unidades del Cretácico Superior, su Relación con las Áreas de Aporte y Evolución de los Medios Sedimentarios, Cuenca del Valle Superior del Magdalena, Colombia. Universidad Nacional de Colombia. |
dc.relation.references | Herrera Quijano, S. (2015). Caracterización Mineralógica de la Formación La Luna , en el Sinclinal del Nuevo Mundo Mediante Difracción de Rayos X (DRX). En Universidad Nacional de Colombia, Trabajos de Grado Geociencias. Universidad Nacional de Colombia. |
dc.relation.references | Hesse, R. (1988). Origin of chert: diagenesis of biogenic siliceous sediments. Diagenesis, 15(3), 227–252. |
dc.relation.references | Hesse, R. (1989). Silica diagenesis: origin of inorganic and replacement cherts. Earth Science Reviews, 26(C), 253–284. https://doi.org/10.1016/0012-8252(89)90024-X |
dc.relation.references | Hettner, A. (1892). La Cordillera de Bogotá. Resultados de Viajes y Estudios. Servicio Geológico Nacional. |
dc.relation.references | Holland, H. D. (2005). Sea level, sediments and the composition of seawater. American Journal of Science, 305(3), 220–239. https://doi.org/10.2475/ajs.305.3.220 |
dc.relation.references | Horton, B. K., Saylor, J. E., Nie, J., Mora, A., Parra, M., Reyes-Harker, A., y 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 |
dc.relation.references | Hubach, E. (1957). CONTRIBUCION A LAS UNIDADES ESTRATIGRAFICAS DE COLOMBIA. En 1212. |
dc.relation.references | Humphries, D. W. (1956). Chert: Its Age and Origin in the Hythe Beds of the Western Weald. Proceedings of the Geologists’ Association, 67(3–4), 296–313. https://doi.org/10.1016/S0016-7878(56)80028-X |
dc.relation.references | Hurd, D. C., y Theyer, F. (1977). Changes in the physical and chemical properties of biogenic silica from the Central Equatorial Pacific: Part II. Refractive Index, Density, and Water Content of Acid-Cleaned Samples. En American Journal of Science (Vol. 277, pp. 1168–1202). |
dc.relation.references | International Commission on Stratigraphy. (n.d.). ICS - Stratigraphic Guide. Retrieved February 19, 2020, from http://www.stratigraphy.org/index.php/icsstratigraphicguide |
dc.relation.references | Jochum, L. M., Chen, X., Lever, M. A., Loy, A., Jørgensen, B. B., Schramm, A., y Kjeldsen, K. U. (2017). Depth Distribution and Assembly of Sulfatereducing Microbial Communities in Marine Sediments of Aarhus Bay. Applied and Environmental Microbiology, 83(23). https://doi.org/10.1128/AEM.01547-17 |
dc.relation.references | Julivert, M. (1968). Lexico Estratigrafico M Julivert (Vol. 5). Centre National de la Recherche Scientifique. |
dc.relation.references | Kastner, M., y Gieskes, J. M. (1983). Opal-A to opal-CT transformation: A kinetic study. Developments in Sedimentology, 36(C), 211–227. https://doi.org/10.1016/S0070-4571(08)70092-X |
dc.relation.references | Kastner, M., Keene, J. B., y Gieskes, J. M. (1977). Diagenesis of Siliceous Oozes- I. Chemical Controls on the Rate of Opal-A to Opal-CT Transformation-an Experimental Study. Geochimica et Cosmochimica Acta, 41(8). https://doi.org/10.1016/0016-7037(77)90099-0 |
dc.relation.references | Knauth, L. P. (1979). A Model for the Origin of Chert in Limestone. Geology, 7(6), 274. https://doi.org/10.1130/0091-7613(1979)7<274:AMFTOO>2.0.CO;2 |
dc.relation.references | Langenheim, R. L. J. (1959). Preliminary report on the stratigraphy of the Giron formation in Santander and Boyaca. Boletín de Geología, 3, 35–50. https://doi.org/10.18273/revbol |
dc.relation.references | Maliva, R. G., y Siever, R. (1989). Nodular Chert Formation in Carbonate Rocks. The Journal of Geology, 97(4), 421–433. https://doi.org/10.1086/629320 |
dc.relation.references | Mckee, E. D., y Weir, G. W. (1953). Terminology for Stratification and Cross-Stratification in Sedimentary Rocks. Bulletin of the Geological Society of America, 64, 381–390. https://doi.org/10.1130/0016-7606(1953)64 |
dc.relation.references | Mojica, J., y Llinas, R. (1984). Observaciones Recientes Sobre las Características del Basamento Económico del Valle Superior del Magdalena en la Región de Payandé-Rovira (Tolima, Colombia), y en Especial sobre la Estratigrafía y Petrografía del Miembro Chicala (= Parte Baja de la Fm. Sa. Geología Colombiana, 13, 81–128. |
dc.relation.references | Mojica, J., y Macia, C. (1981). Características estratigráficas y edad de la Formación Yaví, Mesozoico de la región entre Prado y Dolores, Tolima, Colombia. Geología Colombiana - An International Journal on Geosciences, 12(0), 7–31. |
dc.relation.references | Montoya, D. M., y Reyes, G. A. (2003). Geología de la Plancha 209 Zipaquirá. |
dc.relation.references | Mora, J. a. (2003). Modelo Estratigráfico para el Cretácico Basal (Aptiano-Albiano) en el norte de la Sub-cuenca de Neiva, Valle Superior del Magdalena, Colombia.[PAPER IN. VIII Simposio Bolivariano - Exploracion Petrolera En Las Cuencas Subandinas. http://archives.datapages.com/data/colombia_acggp/simp8/tomo2/Paper85.pdf |
dc.relation.references | Morales, L. G. (1958). General Geology and Oil Occurences of Middle Magdalena Valley, Colombia. SP 18: Habitat of Oil, AAPG Speci(Basin or Areal Analysisor Evaluation), 641–695. https://doi.org/https://doi.org/10.1306/SV18350C25 |
dc.relation.references | Muscente, A. D., Schiffbauer, J. D., Broce, J., Laflamme, M., O’Donnell, K., Boag, T. H., Meyer, M., Hawkins, A. D., Huntley, J. W., McNamara, M., MacKenzie, L. A., Stanley, G. D., Hinman, N. W., Hofmann, M. H., y Xiao, S. (2017). Exceptionally Preserved Fossil Assemblages Through Geologic Time and Space. Gondwana Research, 48, 164–188. https://doi.org/10.1016/j.gr.2017.04.020 |
dc.relation.references | Neuendorf, K. K. E., y American Geological Institute. (2005). Glossary of Geology (J. A. Jackson, J. P. Mehl, y K. K. E. Neuendorf (eds.); 5th ed.). Springer Science y Business Media, 2005. https://books.google.com.co/books?id=SfnSesBc-RgC |
dc.relation.references | North American Commission on Stratigraphic Nomenclature. (2005). North American Stratigraphic Code. AAPG Bulletin, 89(11), 1547–1591. https://doi.org/10.1306/07050504129 |
dc.relation.references | Oehler, J. H. (1975). Origin and Distribution of Silica Lepispheres in Porcelanite From the Monterey Formation of California. JOURNAL OF SEDIMENTARY PETROLOGY, 45(1), 252–257. |
dc.relation.references | Parks, G. A. (1965). The Isoelectric Points of Solid Oxides, Solid Hydroxides, and Aqueous Hydroxo Complex Systems. Chemical Reviews, 65(2), 177–198. https://doi.org/10.1021/cr60234a002 |
dc.relation.references | Patarroyo, P. (2011). Sucesión de Amonitas del Cretácico Superior (Cenomaniano - Coniaciano) de la Parte más Alta de la Formación Hondita y de la Formación Loma Gorda en la Quebrada Bambucá, Aipe - Huila (Colombia, S. A.). Boletin de Geología, 33, 69–92. |
dc.relation.references | Patarroyo, P., y Rojas, A. (2007). La sucesión y la fauna del Turoniano de la Formación San Rafael en Pesca y su comparación con la sección tipo en Samacá ( Boyacá- Turonian succession and fauna of the San Rafael Formation in Pesca and its comparation with the type section in Samaca (Boya. Geología Colombiana, 32(32), 89–96. |
dc.relation.references | Pérez, G., y Salazar, A. (1978). Estratigrafía y Facies del Grupo Guadalupe. Geología Colombiana, 10, 7–86. http://www.revistas.unal.edu.co/index.php/geocol/article/view/30407/30566 |
dc.relation.references | Prauss, M. L. (2015). Marine palynology of the Oceanic Anoxic Event 3 (OAE3, Coniacian - Santonian) at Tarfaya, Morocco, NW Africa - transition from preservation to production controlled accumulation of marine organic carbon. Cretaceous Research, 53, 19–37. https://doi.org/10.1016/j.cretres.2014.10.005 |
dc.relation.references | Raasveldt, H. C., Carvajal, J. M., Buenahora, G., y Servicio Geologico Naciona, M. de minas y petroleos. (1957). Mapa geológico de la plancha K-9 Armero (Edición pr). Servicio Geologico Naciona, Ministerio de minas y petroleos. |
dc.relation.references | Reineck, H. E., y Singh, I. B. (1980). Depositional sedimentary environments, with reference to terrigenous clastics. En Depositional sedimentary environments, with reference to terrigenous clastics. Second edition ( Textbook). (2nd ed.). Springer-Verlag. |
dc.relation.references | Renzoni, G., y Ospina, C. (1969). Geología del cuadrángulo J-12. http://recordcenter.sgc.gov.co/B4/13010010001546/documento/pdf/0101015461102000.pdf |
dc.relation.references | S. W. Wise, K. R. K. (1972). Inferred Diagenetic History of Weakly Silicified Deep-Sea Chalk. AAPG Bulletin, 56. https://doi.org/10.1306/819A4186-16C5-11D7-8645000102C1865D |
dc.relation.references | Sageman, B. (2009). Ocean anoxic events. Encyclopedia of Earth Sciences Series, 185–198. https://doi.org/10.1007/978-1-4020-4411-3_155 |
dc.relation.references | Sagemann, J., Bale, S. J., Briggs, D. E. G., y Parkes, R. J. (1999). Controls on the formation of authigenic minerals in association with decaying organic matter: An experimental approach. Geochimica et Cosmochimica Acta, 63(7–8), 1083–1095. https://doi.org/10.1016/S0016-7037(99)00087-3 |
dc.relation.references | Sarmiento, L. F., Van Wess, J. D., y Cloetingh, S. (2006). Mesozoic transtensional basin history of the Eastern Cordillera, Colombian Andes: Inferences from tectonic models. Journal of South American Earth Sciences, 21(4), 383–411. https://doi.org/10.1016/j.jsames.2006.07.003 |
dc.relation.references | Sarmiento Pérez, G. A., Puentes Ortiz, E. J., y Sierra, C. (2015). Estratigrafía de la Formación La Luna en el Sinclinal de Nuevo Mundo, Valle Medio del Magdalena. Geología Norandina, 12, 24. |
dc.relation.references | Scotese, C. R. (2015). Some Thoughts on Global Climate Change: The Transition from Icehouse to Hothouse. |
dc.relation.references | Spencer, R. J., y Hardie, L. A. (1990). Control of seawater composition by mixing river waters and mid-ocean ridge hydrothermal brines. Fluid-Mineral Interactions: A Tribute to H.P. Eugster, 2(2), 409–419. |
dc.relation.references | Taborda A., B., y Geophysicists., C. S. of P. G. and. (1965). Guidebook to the geology of the De Mares Concession : field trip of February 26-28, 1965. Colombian Society of Petroleum Geologists and Geophysicists. |
dc.relation.references | Taliaferro, N. l. (1934). Contraction Phenomena in Cherts. Geological Society of America Bulletin, 45(2), 189–232. https://doi.org/10.1130/GSAB-45-189 |
dc.relation.references | Terraza, R. (2003). Origen diagenético de Cherts y Porcelanitas en las formaciones Lidita Inferior y Lidita Superior (Grupo Olini), al sur de San Luis (Tolima), Valle Superior del Magdalena, Colombia. Geología Colombiana, 28, 79–94. |
dc.relation.references | Terraza, Roberto. (2020). “Formación la Luna”: expresión espuria en la geología colombiana. En F. Etayo Serna y Comité Editorial Servicio Geológico Colombiano (Eds.), Estudios Geológicos y Paleontológicos sobre el Cretácico en la región del Embalse del Río Sogamoso, Valle Medio del Magdalena (pp. 303–362). Servicio Geológico Colombiano (SGC). |
dc.relation.references | Thorez, J. (1975). Phyllosilicates and Clay Minerals: a Laboratory Handbook for Their X-Ray Diffraction Analysis (G. Lelotte (ed.); Vol. 13, Issue 3). La Universidad de California. https://doi.org/10.1139/t76-035 |
dc.relation.references | Trewin, N. H., y Fayers, S. R. (2005). Sedimentary Rocks | Chert. En Encyclopedia of Geology (pp. 51–62). Elsevier. https://doi.org/10.1016/B0-12-369396-9/00315-4 |
dc.relation.references | Ulloa, C., y Rodriguez, E. (1991). Memoria explicativa Plancha 190. Chiquinquirá (Departamento de Boyacá). |
dc.relation.references | Velandia P., F., Marquinez, A., y Nuñez T., G. (2001). Memoria Explicativa del Mapa Geológico del Departamento del Huila. En Mapa Geológico del Departamento del Huila (Issue Enero). https://doi.org/10.13140/2.1.3373.0885 |
dc.relation.references | Vergara, L., y Rodriguez, G. (1996). Consideraciones sobre la Petrografía y Diagénesis de los Grupos Guadalupe (Cordillera Oriental) y Palmichal (Piedemonte Llanero). Geología Colombiana, 21(1971), 41–63. |
dc.relation.references | Villamil, T. (1998). Chronology, Relative Sea-Level History and a New Sequence Stratigraphic Model for Basinal Cretaceous Facies of Colombia. En Paleogeographic Evolution and Non-Glacial Eustacy, Northern South America (Vol. 58, Issue 58, pp. 161–216). SEPM (Society for Sedimentary Geology). https://doi.org/10.2110/pec.98.58.0161 |
dc.relation.references | Villamil, T., Arango, C., y Hay, W. W. (1999). Plate tectonic paleoceanographic hypothesis for Cretaceous source rocks and cherts of northern South America. En Evolution of the Cretaceous Ocean-Climate System (Vol. 332, Issue August 2009, pp. 191–202). Geological Society of America. https://doi.org/10.1130/0-8137-2332-9.191 |
dc.relation.references | Warren, J. (2000). Dolomite: occurrence, evolution and economically important associations. Earth-Science Reviews, 52(1–3), 1–81. https://doi.org/10.1016/S0012-8252(00)00022-2 |
dc.relation.references | Wheeler, O. (1929). Report on the Palmira series with notes on stratigraphy of the Umir, Lisama, and la Paz formations near the eastern part of the mares concession. Imperial Oil Ltd. |
dc.relation.references | Wilkin, R. T., y Barnes, H. L. (1996). Pyrite formation by reactions of iron monosulfides with dissolved inorganic and organic sulfur species. Geochimica et Cosmochimica Acta, 60(21), 4167–4179. https://doi.org/10.1016/S0016-7037(97)81466-4 |
dc.relation.references | Wilson, R. C. L. (1966). Silica Diagenesis in Upper Jurassic Limestones of Southern England. Journal of Sedimentary Petrology, 36(4), 1036–1049. |
dc.relation.references | Wise, S. W., y Weaver, F. M. (1974). Chertification of Oceanic Sediments. En Pelagic Sediments: On Land and under the Sea (Vol. 1, pp. 301–326). Blackwell Publishing Ltd. https://doi.org/10.1002/9781444304855.ch13 |
dc.relation.references | Wolanski, E., Asaeda, T., y Imberger, J. (1989). Mixing across a lutocline. Limnology and Oceanography, 34(5), 931–938. https://doi.org/10.4319/lo.1989.34.5.0931 |
dc.relation.references | Young, H. R., Li, R., y Kuroda, M. (2012). Silicification in Mississippian Lodgepole Formation, northeastern flank of Williston basin, Manitoba, Canada. Journal of Earth Science, 23(1), 1–18. https://doi.org/10.1007/s12583-012-0229-6 |
dc.rights.accessrights | info:eu-repo/semantics/openAccess |
dc.subject.proposal | Silicificación |
dc.subject.proposal | Cretácico colombiano |
dc.subject.proposal | Geoquímica |
dc.subject.proposal | Zona de sulfatoreducción microbial |
dc.subject.proposal | chert |
dc.subject.proposal | Materia Orgánica |
dc.subject.proposal | sílice |
dc.subject.proposal | Silicification |
dc.subject.proposal | colombian Cretaceous |
dc.subject.proposal | geochemistry |
dc.subject.proposal | microbial sulfatereduction zone |
dc.subject.proposal | organic matter |
dc.subject.proposal | silica |
dc.subject.unesco | Cuenca |
dc.subject.unesco | Roca sedimentaria |
dc.subject.unesco | Materia orgánica |
dc.title.translated | Silicification processes of Turonian - Campanian units in the Cretaceous Colombian Basin |
dc.type.coar | http://purl.org/coar/resource_type/c_bdcc |
dc.type.coarversion | http://purl.org/coar/version/c_ab4af688f83e57aa |
dc.type.content | Text |
dc.type.redcol | http://purl.org/redcol/resource_type/TM |
oaire.accessrights | http://purl.org/coar/access_right/c_abf2 |
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