The Siderian crust (2.47-2.3 Ga) of the Goias Massif and its role as a building block of the Sao Francisco paleocontinent

The basement of the northern Brasilia Belt, in Central Brazil, is dominated by large volumes of TTG magmatism generated during the Early Paleoproterozoic, and represents a continental block formed prior to the welding of the Sao Francisco paleocontinent during the Rhyacian, holding important informa...

Descripción completa

Detalles Bibliográficos
Autores principales: Saboia, Andre Menezes, de Oliveira, Claudinei Gouveia, Dantas, Elton Luiz, Cordeiro, Pedro, Scandolara, Jaime Estevao, Rodrigues, Joseneusa Brilhante, Cordeiro de Sousa, Isabela Moreno
Formato: Artículo (Article)
Idioma:Inglés (English)
Publicado: 2025
Materias:
TTG rocks
Biotite granites and hybrid granitoids
Brasilia Belt
Goias Massif
U-Pb geochronology
Whole-rock geochemistry
13 Climate Action
13 Acción por el clima
Acceso en línea:https://repositorio.uc.cl/handle/11534/100323

Internet

https://repositorio.uc.cl/handle/11534/100323

Ejemplares similares