GEOLOGY, GEOCHEMISTRY AND GEOCRONOLOGY OF THE GRANITIC ROCKS OF SAN IGNÁCIO OROGENY (BOLÍVIA)
Geology, geochemistry and geocronology of the granitic rocks of San Ignácio Orogeny (BOLÍVIA)
DOI:
https://doi.org/10.5016/geociencias.v39i1.12805Abstract
This contribution aims to characterize the Proterozoic granites of San Ignacio orogeny, western Bolivia, describing their chemical composition, U-Pb and Sm/Nd isotopic to identify sources and process of the crustal formation. The results of chemical and isotopic granitoids of Cachuela, Motacusal and Talcoso, present U/Pb age in zircon between 1307 and 1333 Ma, suggesting an important epoch of generation of granitoids in the Bolivian pre-Cambrian. Chemistry (A-Type granites) and Nd isotopes (εNd(1330) between -0.77 and -3.86) signatures here reported suggest an anorogenic environment and the spider diagram indicate the within-plates tectonic setting for the formation of these granites, instead of arc-related environment is suggested in the literature for these rocks. The data here reported suggest a geological evolution for the Bolivian pre-Cambrian composed of the San Ignacio event is represented by magmatic arc with participation of continental crust previously formed representing an important collisional period in the SW Amazonian craton.