Vol. 30 No. 2 (2008): Boletín De Geología
Articles

ROCAS CON AFINIDAD ADAKITICA AL SUR-ESTE DE MANIZALES: RASGOS PETROGENETICOS Y GEOQUIMICOS

Luz Mary Toro Toro
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Mauricio Alvarán-Echeverri
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Carlos Alberto Borrero-Peña
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How to Cite

Toro Toro, L. M., Alvarán-Echeverri, M., & Borrero-Peña, C. A. (2008). ROCAS CON AFINIDAD ADAKITICA AL SUR-ESTE DE MANIZALES: RASGOS PETROGENETICOS Y GEOQUIMICOS. Boletín De Geología, 30(2). Retrieved from https://revistas.uis.edu.co/index.php/revistaboletindegeologia/article/view/40

Abstract

 

To the southeast of Manizales city, in Gallinazo area, there are a series of aligned hills such as: Gallinazo, Amazonas, Sabinas, La Oliva and La Negra, corresponding to volcanic and sub-volcanic rocks of  andesitic and dacitic composition respectively, geochemical data present characteristic of adakitic rocks. 

Both, volcanic and sub-volcanic rocks presents high SiO2 concentration (63,87-70,15%), Al2O3 (14,18-16,83%), low Y concentration (11,20-27 ppm) and Yb (0,94-1,93 ppm); strong enrichment in Light Rare Earth Elements(LREE) and highly incompatible elements (Rb, Ba), except for Sr which presents low contents and negative anomaly of Nb-Ta, characteristic that distinguish also the calcoalkaline magmas. Geochemical pattern of LREE and multielements show a strong fractionation ((La/ Yb)n>8) with typical low content of (Yb ≤ 1.8 ppm , Y ≤ 18 ppm). 

In this work authors propose SE Manizales adakita-like rocks were generated by subducted basaltic slab melting with some minimum peridotitic mantelic wedge contamination. Genesis and geochemical characteristics of these rocks open the possibility to find Au-Cu porphyry mineralizations and epithermal gold deposits in this area due to their highly oxidixing potential. 

Keywords: adakita-like rocks, subduction, volcanic rocks, Manizales, Colombia.

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