Vol. 38 No. 3 (2016): Boletín de Geología
Articles

PETROGRAPHY AND CARTOGRAPHY OF CONTACT AUREOLE OF THE MARIQUITA GRANODIORITE (TOLIMA DEPARTMENT, COLOMBIAN CENTRAL CORDILLERA)

Sergio Andrés Celis
Instituto de Investigaciones en Estratigrafía IIES , Universidad de Caldas. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas.
Carlos Ariel Giraldo-Villegas
Instituto de Investigaciones en Estratigrafía IIES , Universidad de Caldas. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas.
Luz Mary Toro-Toro
Instituto de Investigaciones en Estratigrafía IIES , Universidad de Caldas. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas.
Edward Osorio Granada
Instituto de Investigaciones en Estratigrafía IIES , Universidad de Caldas. Facultad de Ciencias Exactas y Naturales. Departamento de Ciencias Geológicas.

Published 2016-07-01

Keywords

  • contact aureole,
  • Mariquita,
  • Colombia

How to Cite

Celis, S. A., Giraldo-Villegas, C. A., Toro-Toro, L. M., & Granada, E. O. (2016). PETROGRAPHY AND CARTOGRAPHY OF CONTACT AUREOLE OF THE MARIQUITA GRANODIORITE (TOLIMA DEPARTMENT, COLOMBIAN CENTRAL CORDILLERA). Boletín De Geología, 38(3), 31–40. https://doi.org/10.18273/revbol.v38n3-2016002

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Abstract

In the Department of Tolima, northwest of the town of Mariquita, crops out the Mariquita Granodiorite, which known age is 113 ± 4 Ma K-Ar in biotite. The intrusive contact with the green, gray and black schists of the Cajamarca Complex developed a clear contact aureole with a maximum width of approximately 520 m in the area of Medina Falls (Mariquita-La Victoria road), which extends to the Chiminá creek, where its extent is reduced to approximately 240 m. Quartz-biotite and quartz-actinolite hornfels were developed as a superimposed event to a previous regional and ductile metamorphism. The albite-epidote hornfels facies is determined by the actinolite-epidote-chlorite association.

 

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