Relaciones isotópicas Sm/Nd en rocas graníticas y miloníticas de Sierras Pampeanas del noroeste Argentino
DOI:
https://doi.org/10.3989/egeol.05611-236Keywords:
Pampean Ranges, Northwestern Argentina, Famatinian Cycle, TIPA shear zone, Sm/Nd ageAbstract
The Velasco, Copacabana and Paimán Ranges in Sierras Pampeanas, are constituted mainly by paleozoic plutonic bodies of the Famatinian cycle (Huaco, Antinaco and Paimán) and for mylonitic rocks (TIPA Shear Zone), originated as a consequence of dynamic events happening during the Upper Ordovician-Devonian. The last magmatic event of the area would probably have of devonian age (Granite San Blas). Model-ages of two stages were calculated based on 147Sm/144Nd relationships; the obtained values are closely grouped at around 1594 Ma. and the more plausible interpretation seems to be a reworking of an Early Proterozoic protolith.
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Published
2005-04-30
How to Cite
López, J. P., Rodríguez Areal, M. M., Sales, A., & Kawashita, K. (2005). Relaciones isotópicas Sm/Nd en rocas graníticas y miloníticas de Sierras Pampeanas del noroeste Argentino. Estudios Geológicos, 61(1-2), 3–8. https://doi.org/10.3989/egeol.05611-236
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