@article{10272/13379,
year = {1995},
url = {http://hdl.handle.net/10272/13379},
abstract = {The fluorite mineralization from the La Nueva Mine, has a S m-Nd age of 130±19 Ma, and thus must be related to the Lower Cretaceous late -Gondwanic extensional and magmatic event that affected the Sierras Pampeanas Basement of Argentina. Hydrothermal fluids involved in the formation of fluorite were probably derived by mixing of two fluids , an ascending high B7Sr/86Sr one, probably equilibrated with basement metamorphics, as suggested by the very negative ENd(130) values, and a second, «descending», with a low B7Sr/86Sr value},
publisher = {Sociedad Geológica de España},
title = {Edad y origen de la fluorita del yacimiento de La Nueva (Cabalango, Córdoba, Argentina) en base a geoquímica de isótopos radiogénicos (Nd y Sr)},
title = {Age and origin of the «La Nueva» fluorite lode (Cabalango, Cordoba, Argentina) based on radiogenic isotope (Nd, Sr) geochemistry},
author = {Galindo, Carmen and Baldo, Edgardo G. and Pankhurst, R. J. and Casquet Martín, César and Rapela, C. and Saavedra, J.},
}