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Zorano Srgio de Souza Jean-Marc Montel Simone Maria Lima Costa Gioia Maria Helena Bezerra Maia de Hollanda Marcos Antonio Leite do Nascimento Emanuel Ferraz Jardim de S Venerando Eustquio Amaro Mrcio Martins Pimentel Jean-Marc Lardeaux Michelle Veschambre 《Gondwana Research》2006,9(4):441-455
The easternmost domain of the Borborema Province, northeastern Brazil, presents widespread, extensional-related high-temperature metamorphism during the Brasiliano (=Pan-African) orogeny. This event reached the upper amphibolite to granulite facies and provoked generalized migmatization of Proterozoic metapelitic rocks of the Seridó Group and tonalitic to granodioritic orthogneisses of the Archean to Paleoproterozoic basement. We report new geochronological data based on electron microprobe dating of monazite from metapelitic migmatite and leuconorite within the high-T shear zones that make up the eastern continuation of the huge E–W Patos shear belt. These data were also constrained by using the Sm–Nd isotopic systematic on garnet from a syntectonic alkaline granite and two garnet-bearing leucosomes. The results suggest an age of about 578 to 574 Ma for the peak of the widespread high-T metamorphism. This event is best recorded by Sm–Nd garnet-whole rock ages. The U–Th–Pb isotopes on monazite of the metapelitic migmatite show a younger thermal event at 553 ± 10 Ma. When compared to the Sm–Nd garnet-whole rock ages, the U–Th–Pb electron probe monazite ages seem to record an event of slightly lower temperatures after the peak of the high-T metamorphism. This may reflect the difference in the isotopic behavior of the geochronological methods employed. Otherwise, the U–Th–Pb ages on monazites could indicate an event not yet very well defined. In anyway, this paper reveals the partial or even complete re-opening and resetting of the U–Th–Pb isotopic system produced by the action of low-T Ca-rich fluid. 相似文献
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Dimitri Alexei Gadotti Ronaldo Eustáquio de Souza 《Astrophysics and Space Science》2003,284(2):527-530
To further enhance our understanding on the formation and evolution of bars in lenticular (S0) galaxies, we are undertaking
a detailed photometric and spectroscopic study on a sample of 22 objects. Here we report the results of a 2D structural analysis
on two barred face-on S0's, which indicate that presently these galaxies do not possess disks. We discuss two possibilities
to explain these surprising results, namely strong secular evolution and bar formation without disks.
This revised version was published online in August 2006 with corrections to the Cover Date. 相似文献
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