E. Koester et al., SHRIMP U-Pb age for the emplacement of the Santana Granite and reactivation of the Porto Alegre Suture, southern Brazil, J S AM EART, 14(1), 2001, pp. 91-99
SHRIMP U-Pb zircon ages are reported from a sample of the Santana Granite t
hat represents the beginning of alkaline magmatic activity in the Neoproter
ozoic of the Sul-Rio-Grandense Shield, Brazil. This granite outcrops in the
city of Porto Alegre and has a NE-SW elongated shape (20 km long and 5 km
wide). It is a medium- to coarse-grained syenogranitic rock with subvertica
l magmatic foliation and subhorizontal lineation with NE-SW trends, overpri
nted by a weak solid-state fabric. Zircons of this rock with (206)Pp/U-238
ages between ca. 575 and ca. 617 Ma are interpreted as having formed during
magmatic crystallisation; the best fit for this age using five analyses pr
ovided a mean (206)pb/U-238 age of 600 +/- 10 Ma. This age is also interpre
ted as the age of the reactivation of the Porto Alegre Suture, a crustal di
scontinuity along which the Santana Granite was emplaced. Younger isotopic
data (< 575 Ma) for zircons from this sample are interpreted as due to Pb l
oss from metamietization. The 600-Ma age is consistent with previous result
s and marks a magmatic episode, probably related to an extensional tectonic
episode that affected the NE of the Sul-Rio-Grandense Shield at the end of
the Brasiliano Cycle. (C) 2001 Elsevier Science Ltd. All rights reserved.