Petrología y geoquímica  de los granitoides peralumínicos de la Faja TIPA, en el borde occidental de Gondwana, sistema de Famatina, Argentina

J. P. López; A. J. Toselli

doi:10.3989/egeol.96523-4257

Petrología y geoquímica de los granitoides peralumínicos de la Faja TIPA, en el borde occidental de Gondwana, sistema de Famatina, Argentina

Authors

J. P. López Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán
A. J. Toselli Instituto Superior de Correlación Geológica. Universidad Nacional de Tucumán

DOI:

https://doi.org/10.3989/egeol.96523-4257

Keywords:

Petrology, geochimistry, peralumic, granitoids, Famatina, Argentina

Abstract

Main pretrological and geochemistry characteristics of the rocks of Copacabana, Paimán and Velasco Ranges are shown, constituent of the important deformative structure developed in the east border of Famatinian System. This structure is relationed with Ocloyic-Taconic Collision between Gondwana and Laurentia, during Upper Ordovicic-Lower Siluric and Lower Carbonic, in response to a compressive regimen with vergence to the East.

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Published

1996-08-30

How to Cite

López, J. P., & Toselli, A. J. (1996). Petrología y geoquímica de los granitoides peralumínicos de la Faja TIPA, en el borde occidental de Gondwana, sistema de Famatina, Argentina. Estudios Geológicos, 52(3-4), 97–102. https://doi.org/10.3989/egeol.96523-4257

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Issue

Vol. 52 No. 3-4 (1996)

Section

Articles

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