Abstract (EN):
The determination of absolute ages by isotopic systematics is an indispensable datum to constrain the petrogenesis and evolution conditions of a rock, being a contribution to a better characterization of the geological and tectonic settings. The granitic rocks of Porto region have been the object of several isotopic and geochronological studies that have allowed a comparative approach by different methods, namely U-Pb, Rb-Sr and Sm-Nd. The age determination of the Porto peraluminous two-mica granite by the Rb-Sr systematics based on recent estimates of the 87Rb decay constant, assumed as more accurate than the constant usually recommended, suggests the age of 311±7 Ma for the emplacement of the Porto granite. This age is in agreement with the affiliation of Porto granite to the group of syn-tectonic granites related with the third Hercynian deformation phase. The present results are more concordant with the U-Pb ages reported in previous works for zircon and monazite of the same granite. © 2015 LNEG - Laboratório Nacional de Geologia e Energia IP.
Language:
Portuguese
Type (Professor's evaluation):
Scientific