Structural style and evolution of the offshore portion of the Sinu Fold Belt (South Caribbean Deformed Belt) and adjacent part of the Colombian Basin

[EN] The Sinu fold belt, located in northwestern Colombia, is the southwesternmost part of the South Caribbean Deformed Belt, which has been interpreted as an accretionary wedge resulting from the subduction of the Caribbean Plate under the South American Plate. The geological interpretation of 2D s...

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Detalles Bibliográficos
Autores: Rodríguez Álvarez, Indira, Bulnes Cudeiro, María Teresa, Poblet Esplugas, Josep, Masini, Massimiliano, Flinch, Joan F.
Tipo de recurso: artículo
Estado:Versión publicada
Fecha de publicación:2021
País:España
Institución:Universidad de León
Repositorio:BULERIA. Repositorio Institucional de la Universidad de León
OAI Identifier:oai:buleria.unileon.es:10612/26773
Acceso en línea:https://www.sciencedirect.com/science/article/pii/S0264817220306450
https://hdl.handle.net/10612/26773
Access Level:acceso abierto
Palabra clave:Geología
Sinu Fold Belt
Colombian basin
Thrust-related folds
Normal faults
Shale diapirs
2506.20 Geología Estructural
Descripción
Sumario:[EN] The Sinu fold belt, located in northwestern Colombia, is the southwesternmost part of the South Caribbean Deformed Belt, which has been interpreted as an accretionary wedge resulting from the subduction of the Caribbean Plate under the South American Plate. The geological interpretation of 2D seismic surveys and bathymetric maps, with the aid of a few exploration wells, has been the basis to construct a structural map and several geological sections to illustrate the offshore part of the Sinu Fold Belt and the portion of the Colombian Basin adjacent to the belt. Their analysis has allowed us to characterize different structural styles (thrusts and related folds in the outer part of the belt, and normal faults and shale diapirs in the inner one), the timing of the structures, as well as the kinematic evolution from a Cretaceous-Paleocene extensional event responsible for the Colombian Basin structure to the Pliocene-Quaternary contractional event which caused the Sinu Fold Belt