Vol. 35 No. 1 (2013): Boletín de Geología
Articles

PETROGRAPHY, GEOCHEMISTRY AND AGE OF THE FARALLONES GRANODIORITE AND ASSOCIATED VOLCANIC ROCKS

Gilberto Zapata García
Servicio Geológico Colombiano GTR Medellín
Bio
Gabriel Rodríguez García
Servicio Geológico Colombiano GTR Medellín
Bio

Published 2013-05-31

How to Cite

Zapata García, G., & Rodríguez García, G. (2013). PETROGRAPHY, GEOCHEMISTRY AND AGE OF THE FARALLONES GRANODIORITE AND ASSOCIATED VOLCANIC ROCKS. Boletín De Geología, 35(1). Retrieved from https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/3228

Abstract

The Farallones Granodiorite is located on the western flank of the  Cordillera Occidental of Colombia, is formed by tonalite, granodiorite, quarz diorite, monzodiorite, quarz monzodiorite, diorite, gabbro and quarz monzonite. The content of silica in the rocks varies between 67.76 and 52,07%, the body is not homogeneous and there are alkaline rocks in the southern part of the body and subalcalines in the northern sector of the pluton. There are rich rocks K2O ranging from medium K to shoshonitic series, they are metaluminous but near the edges of the pluton they are peraluminous due to contamination by sediments.

The Farallones Granodiorite correspond to midly evolved magmas with impoverishment of HREE8 respect to LREE,  that correspond  to a pluton formed in an arc enviroment. The age of the Farallones Granodiorite  in hornblende for the  method K/Ar 11± 2 Ma (Calle et al., 1980a) and two in Arboleda et al. (2009) by the method Ar/Ar 11.9 and 9. 8± 0.2, which correspond to the Late Miocene. This geological unit intrudes the Sandstones, siltstones and mudstones of Penderisco, and in turn, it is intruded by the diatremic brecchas of Farallones.

Keywords: Farallones Granodiorite, Cordillera Occidental of Colombia, Farallones diatremic breccia

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References

Arboleda, G., Celada, C., Forero, S., Montealegre, V., Carmona, J., y Medina, E. 2009. Cartografía geológica y muestreo geoquímico en la parte norte de la Cordillera Occidental, planchas 165 y 185 (396 kilómetros cuadrados). Contrato No. 392 de 2007 INGEOMINAS-UTAGS-GE. Bogotá. 178p

Best, M.G. 2003. Igneous and metamorphic petrology: Second edition. Oxford Blackwell Science, 729p

Calle, B., Toussaint, J., Restrepo, J., y Linares, E. 1980a. Edades K/Ar de dos plutones de la parte septentrional de la Cordillera Occidental, Colombia. Geología Norandina, 2:17-20.

Calle, B., González, H., De La Peña, R., Escorce, B., y Durango, J. 1980b. Mapa geológico de la Plancha 186 Riosucio. Escala 1:100.000 INGEOMINAS, Bogotá

Calle, B., y Salinas, R. 1986. Geología y Geoquímica de la Plancha 165 Carmen de Atrato. INGEOMINAS. Bogotá, Informe 1967, 140p.

CORPORACIÓN AUTONOMA REGIONAL DEL CENTRO DE ANTIOQUIA-UNIVERSIDAD NACIONAL DE COLOMBIA. 1997. Reserva natural “Farallones del Citará” – estudios biofísicos y socioeconómicos preliminares- (Suroeste Antioqueño). Informe Técnico, Tomo II: 70-71

Cox, K.G., Bell, J.D., and Pankhurst, R.J. 1979. The interpretation of igneous rocks. Georgen Allen and Unwin, London

González, H., y Londoño, A. 2002. Catálogo de unidades litoestratigráficas de Colombia. Mioceno. Monzodiorita de Farallones (Nmdf), departamentos de Antioquia, Chocó y Risaralda, Cordillera Occidental. INGEOMINAS, 17p.