The western Sao Francisco pericraton interpreted from crustal magnetic and gravity sources

The Neoproterozoic Brasiliano Orogeny shaped the former Sao Francisco paleocontinent into a preserved cratonic nucleus surrounded by a pericratonic region. In central Brazil, this pericraton crops out as the Goias Massif, the basement of the northern Brasilia Belt. The well-known difficulty of traci...

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Detalles Bibliográficos
Autores principales: Oliveira dos Reis, Luciane Katiuscia, Vidotti, Roberta Mary, Cordeiro, Pedro, de Oliveira, Claudinei Gouveia
Formato: Artículo (Article)
Idioma:Inglés (English)
Publicado: 2025
Materias:
Acceso en línea:https://repositorio.uc.cl/handle/11534/100422