Artículos científicos
Proveniencia de la Formación Ciénaga de Oro: revelando la evolución tectónica del margen Caribe colombiano durante el Oligoceno - Mioceno Temprano
Alejandra Manco-Garcés- Maria Isabel Marín-Cerón
- Carlos Javier Sánchez-Plazas
- Luis Carlos Escobar-Arenas
- Alejandro Beltrán-Triviño
- Albrecht von-Quadt
Publicado 2020-09-30
Palabras clave
- Formación Ciénaga de Oro,
- Cinturón Plegado San Jacinto,
- Proveniencia,
- Minerales pesados,
- Paleocorrientes
- Norte de la placa suramericana ...Más
Cómo citar
Manco-Garcés, A., Marín-Cerón, M. I., Sánchez-Plazas, C. J., Escobar-Arenas, L. C., Beltrán-Triviño, A., & von-Quadt, A. (2020). Proveniencia de la Formación Ciénaga de Oro: revelando la evolución tectónica del margen Caribe colombiano durante el Oligoceno - Mioceno Temprano. Boletín De Geología, 42(3), 205–226. https://doi.org/10.18273/revbol.v42n3-2020009
Derechos de autor 2020 Boletín de Geología
Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.
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Resumen
Se realizó el estudio de una sección estratigráfica en el Cinturón Plegado y de Cabalgamiento de San Jacinto, localizado en el noroccidente de Colombia. En esta sección aflora parte de la Formación Ciénaga de Oro del Oligoceno-Mioceno temprano. Este trabajo analiza la procedencia de los sedimentos, utilizando un enfoque de múltiples herramientas que incluye: (I) conteo de clastos de areniscas y conglomerados con malla, (II) minerales pesados, y (III) paleocorrientes y (IV) edades U-Pb de circones detríticos. La secuencia sedimentaria fue depositada en un ambiente deltaico a transicional, con reducción del efecto del oleaje y la marea junto con el incremento de la dominancia de los procesos transicionales de río hacia el tope de la sección. Se identificó dos áreas fuentes de una provincia de arco disectado: principalmente un área fuente de composición granítica a pegmatítica y un área fuente secundaria de composición ígnea a básica, localizadas al este y suroeste de la posición actual de la secuencia. El análisis geocronológico de circones detríticos muestra cuatro poblaciones de edades: (I) Devónico-Pérmico, (II) Pérmico-Triásico, (III) Jurásico y (IV) Cretácico. Las edades máximas de depositación corresponden a 75,2±0,9 Ma en la parte más baja de la sección, 68,9±0,6 Ma en el medio y 74,5±0,7 Ma para la parte superior de la sección. Se propone que el material depositado en COF fue suministrado desde sistemas fluviales del sur hacia el norte, que erosionaron bloques de basamento expuesto y su cobertura sedimentaria (Cretácico tardío a Paleógena) durante el Oligoceno. Este sistema fluvial transportó sedimentos desde plutones tipo Batolito Antioqueño del Cretácico Tardío y rocas máficas/ultramáficas, como las encontradas en las Cordillera Central y Occidental.
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