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1016/0895-9811(91)90003-4. , 1997, The Mara Rosa arc in the Tocantins Province: Further evidence for Neoproterozoic crustal accretion in central Brazil: Precambrian Research, v. 81, p. 1016/S0301-9268(96)00039-3. , 1999, Granites and the geodynamic history of the Neoproterozoic Brasília belt, central Brazil: A review: Lithos, v. 46, p. 1016/S0024-4937(98)00078-4. , 1990, Relações embasamento-cobertura na porção occidental do Cinturão Dom Feliciano: Um esboço estrutural: Pesquisas, v. 17, p. 72–84.

1992, O Magmatismo Granítico da região Oriental do Escudo Sul-rio-grandense. Uma Revisão: Pesquisas, v. 19, p. 183–189. , 1999, Relações isotópicas Rb-Sr e Sm-Nd e idades do magmatsimo granítico Brasiliano da região leste do cinturão Dom Feliciano no Rio Grande do Sul: Evidêcias de retrabalhamento de crosta continental Paleoproterozóica: Revista Brasileira de Geociências, v. 29, p. 227–232. , 2000, Geological units, ages and tectonic evolution of the Neoproterozoic Dom Feliciano belt, southernmost Brazil—A review: Revista Brasileiras de Geociências, v.

They outpoured from an important N 30°-trending fissural system over a basin floor. Some lherzolite fragments have been sliced along southwest-northeast faults, in the Lower Cambrian sediments. They originated from a transitional mantle between continental and oceanic domains. fr. , The evolution of the Rheic Ocean: From Avalonian-Cadomian active margin to Alleghenian-Variscan collision: Geological Society of America Special Paper 423, p. 2423(02). org. ©2007 Geological Society of America. All rights reserved.

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