Boletín de Geología

Vol. 46 Núm. 3 (2024): Boletín de Geología
Homenaje al trabajo del Dr. Gerardo Botero-Arango

Algunas consideraciones sobre la estructura sísmica cortical en el norte de la Cordillera Central colombiana - Altiplano Antioqueño

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  • Gaspar Monsalve,
  • Andrés F. Muñoz-Calderón,
  • David Santiago Avellaneda-Jiménez,
  • Sebastián Ramírez-Flórez
Gaspar Monsalve
Universidad Nacional de Colombia
Andrés F. Muñoz-Calderón
Universidad Nacional de Colombia
David Santiago Avellaneda-Jiménez
Carnegie Institution for Science
Biografía
Sebastián Ramírez-Flórez
Universidad Nacional de Colombia
DOI: https://doi.org/10.18273/revbol.v46n3-2024011

Publicado 2024-11-28

Palabras clave

  • Altiplano Antioqueño,
  • Batolito Antioqueño,
  • Espesor cortical,
  • Función receptora,
  • Sismicidad,
  • Mecanismo focal
    • ...Más
    Menos

Cómo citar

Monsalve, G., Muñoz-Calderón, A. F., Avellaneda-Jiménez, D. S., & Ramírez-Flórez, S. (2024). Algunas consideraciones sobre la estructura sísmica cortical en el norte de la Cordillera Central colombiana - Altiplano Antioqueño. Boletín De Geología, 46(3), 247–263. https://doi.org/10.18273/revbol.v46n3-2024011

Derechos de autor 2024 Boletín de Geología

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Esta obra está bajo una licencia internacional Creative Commons Atribución 4.0.

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Resumen

En la parte norte de la Cordillera Central colombiana se encuentra el Altiplano Antioqueño, un conjunto de superficies de erosión geológicamente dominado por las rocas intrusivas del Batolito Antioqueño. La naturaleza de la deformación de la corteza en esta zona es aún enigmática. En este trabajo se integran algunos elementos que pueden contribuir al entendimiento de la estructura sísmica de la corteza, incluidos el uso de la técnica sismológica de la función receptora para estimar espesor cortical, el análisis de la sismicidad instrumental, y el cálculo de mecanismos focales de sismos con magnitudes mayores a 3; la integración de estos con el conocimiento de las litologías y las fallas regionales, permiten una mejor aproximación a la estructura cortical y a las características de su deformación actual. En particular, las funciones receptoras telesísmicas indican espesores de corteza de entre 45 y 55 km, sobre todo en el flanco occidental del altiplano; las funciones receptoras no son concluyentes acerca de este espesor en vecindades de su límite oriental. La sismicidad instrumental muestra una acumulación de sismos en los alrededores del Batolito Antioqueño y una relativa ausencia de estos en su interior. Los mecanismos focales indican un fallamiento inverso en el borde occidental del batolito y fallamientos de rumbo cercanos a su borde oriental.

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