Jurassic break-up of the Peri-Gondwanan margin in northern Colombia: Basin formation and implications for terrane transfer
Jurassic extensional basins developed along the northwestern margin of South America during the break-up of Pangea. Presently, these basins are dispersed in several tectonic blocks of the northern Andes and Mexico, hindering reconstruction of western equatorial Pangea before break-up. This is the ca...
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2019
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| 001 | PAPER-25866 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205801.0 | ||
| 008 | 190410s2019 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85056800746 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Nova, G. | |
| 245 | 1 | 0 | |a Jurassic break-up of the Peri-Gondwanan margin in northern Colombia: Basin formation and implications for terrane transfer |
| 260 | |b Elsevier Ltd |c 2019 | ||
| 270 | 1 | 0 | |m Nova, G.; Corporación Geológica ARES, Calle 26 N. 69C-03 Torre C of. 904, Colombia; email: gnova@cgares.org |
| 506 | |2 openaire |e Política editorial | ||
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| 504 | |a Zuluaga, C., Ochoa, A., Muñoz, C., Guerrero, N., Martínez, A., Medina, P., Pinilla, A., Zapata, V., Cartografía e historia geológica de la Alta Guajira, implicaciones en la búsqueda de recursos minerales, acuerdo específico 030 de 2006 (2009), p. 536. , Ingeominas-Universidad Nacional de Colombia sede Bogotá; Zuluaga, C.A., Pinilla, A., Mann, P., Jurassic silicic volcanism and associated continental-arc basin in Northwestern Colombia (southern boundary of the Caribbean plate) (2015) Petroleum Geology and Potential of the Colombian Caribbean Margin: AAPG Memoir 108, pp. 137-160. , C. Bartolini P. Mann | ||
| 504 | |a Zuluaga, C.A., Amaya, S., Urueña, C., Bernet, M., Migmatization and low-pressure overprinting metamorphism as record of two pre-Cretaceous tectonic episodes in the Santander Massif of the Andean basement in northern Colombia (NW South America) (2017) Lithos, 274-275, pp. 123-146 | ||
| 520 | 3 | |a Jurassic extensional basins developed along the northwestern margin of South America during the break-up of Pangea. Presently, these basins are dispersed in several tectonic blocks of the northern Andes and Mexico, hindering reconstruction of western equatorial Pangea before break-up. This is the case of the Cosinas Basin (Guajira block) and the Machiques Basin (Perijá Range), in northern Colombia, which are filled by Jurassic sedimentary and volcano-sedimentary successions. Autochthonous and para-autochthonous hypotheses on the origin of this basins have been proposed. The purpose of this research is to document the sedimentological evolution, depositional age (Sr-isotope + U-Pb geochronology), sediment provenance and paleogeography of the Cosinas and Machiques basins in order to constrain whether these basins formed within a single extensional margin or they formed as extensional basins in different tectonic blocks. Volcanic detrital zircon U-Pb ages documented in La Quinta Formation in the Machiques Basin and at the base of Rancho Grande Formation in the Cosinas Basin suggest that extensional basins were active in Early Jurassic time. However, a significant difference exists in their subsequent history. Whereas in the Machiques Basin dominates the accumulation of Lower and Middle Jurassic volcanoclastic deposits with abrupt lateral thickness changes, accumulation in the Cosinas Basin is dominantly of siliciclastic strata, with the record of two major marine incursions in Late Jurassic time. Integration of provenance results indicates that the Santander Massif supplied sediments to the Machiques Basin. In contrast, Middle to Upper Jurassic sandstones of the Cosinas Basin document unroofing of basement blocks that include metamorphic, sedimentary and plutonic rocks from the Guajira and Maya blocks. The similarity in age and composition of pre-Jurassic rocks in northwestern South America and the so-called peri-Gondwana blocks in the Mexican subcontinent (i.e., Maya and Oaxaquia blocks) challenge the use of detrital zircon population as an indicator of the autochthonous or para-autochthonous origin of the Guajira block. Large uncertainty of paleomagnetic results, and the lack of constraints for the time magnetization acquisition preclude estimating paleolatitudes for the Guajira block in Jurassic time but support previous interpretation of ca. 70°-90° clockwise rotation of the Guajira block relative to stable South America craton. Our preferred paleogeography considers that the Cosinas and Machiques basins were close to each other along the western continental margin of Pangea during the onset of extension in Early Jurassic time. The change from continental to marine depositional environments in Middle to Late Jurassic time along the Cosinas Basin, which have not been identified in the Machiques Basin or other autochthonous Jurassic basins in northwestern South America, allow us to propose that these blocks were separated during the Callovian - Tithonian interval, with the Cosinas Basin remaining closer to a conjugate Mexican margin, that we interpret as the Maya block. Collision of the Guajira block with the South American margin occurred near the Jurassic-Cretaceous boundary, as documented by deformation of Jurassic units previous to deposition of Berriasian strata in the Guajira block. © 2018 Elsevier Ltd |l eng | |
| 536 | |a Detalles de la financiación: Smithsonian Tropical Research Institute, 727771451027 | ||
| 536 | |a Detalles de la financiación: Field work in 2010, 2011, 2012 seasons in Guajira and Perijá Ranges as well as geochronology and paleomagnetism laboratory analyses were funded by several institutes ( Ecopetrol ,Colombia; OGX , Colombia; STRI, Panama and ARES, Colombia ) under diverse projects. Colciencias supplied partial funding to GN and PM as part of the Jovenes Investigadores programme during 2011 and 2012, and field work and Sr Isotopes analyses during 2016–2017 under the project 727771451027 “ Quantifying the effects of Ocean Acidification and Deoxygenation on the marine biogeochemical cycles during periods of high atmospheric PCO 2 : Implications for the future of the 21st Century Oceans” . Collaboration from staff of the Paleomagnetic Laboratory Daniel A. Valencio from IGEBA is appreciated. The indigenous Wayu communities from the Guajira and Perijá areas are thanked for their collaboration during all field seasons. Reviews and suggestions by Roberto Molina Garza, James Pindell and an anonymous reviewer improved the manuscript and it are thanked Appendix A | ||
| 593 | |a Corporación Geológica ARES, Calle 26 N. 69C-03 Torre C of. 904, Bogotá, Colombia | ||
| 593 | |a Testlab Geoambiental, Carrera 45 D # 60-16, Medellín, Colombia | ||
| 593 | |a Facultad de Minas, Universidad Nacional de Colombia, Medellín, Colombia | ||
| 593 | |a IGEBA, Universidad de Buenos Aires, Buenos Aires, Argentina | ||
| 593 | |a Helmholtz Centre for Ocean Research Kiel Geomar, Kiel, Germany | ||
| 593 | |a Instituto de Investigaciones Estratigráfica, Universidad de Caldas, Manizales, Colombia | ||
| 593 | |a Department of the Environment, Washington State University, Pullman, United States | ||
| 593 | |a ECOPETROL, Bogotá, Colombia | ||
| 593 | |a Departamento de Fisica y Geociencias, Universidad del Norte, Barranquilla, Colombia | ||
| 593 | |a Faculty of Sciences, Antonio Nariño University, Circunvalar campus, Bogota, Colombia | ||
| 690 | 1 | 0 | |a COSINAS BASIN |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a MACHIQUES BASIN |
| 690 | 1 | 0 | |a PERI-GONDWANA |
| 690 | 1 | 0 | |a PROVENANCE |
| 690 | 1 | 0 | |a BASIN EVOLUTION |
| 690 | 1 | 0 | |a CONTINENTAL BREAKUP |
| 690 | 1 | 0 | |a CONTINENTAL MARGIN |
| 690 | 1 | 0 | |a DEPOSITIONAL ENVIRONMENT |
| 690 | 1 | 0 | |a GEOCHRONOLOGY |
| 690 | 1 | 0 | |a GONDWANA |
| 690 | 1 | 0 | |a JURASSIC |
| 690 | 1 | 0 | |a PALEOGEOGRAPHY |
| 690 | 1 | 0 | |a PROVENANCE |
| 690 | 1 | 0 | |a SEDIMENTARY SEQUENCE |
| 690 | 1 | 0 | |a SEDIMENTOLOGY |
| 690 | 1 | 0 | |a TERRANE |
| 651 | 4 | |a COLOMBIA | |
| 700 | 1 | |a Bayona Chaparro, G.A. | |
| 700 | 1 | |a Silva-Tamayo, J.C. | |
| 700 | 1 | |a Cardona, A. | |
| 700 | 1 | |a Rapalini, A. | |
| 700 | 1 | |a Montaño Cortes, P.C. | |
| 700 | 1 | |a Eisenhauer, A. | |
| 700 | 1 | |a Dussan, K.T. | |
| 700 | 1 | |a Valencia, V.A. | |
| 700 | 1 | |a Ramirez, V. | |
| 700 | 1 | |a Montes, C. | |
| 773 | 0 | |d Elsevier Ltd, 2019 |g v. 89 |h pp. 92-117 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
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