Source of the synkinematic magmatism in the Dorsal de Canguçu Transcurrent Shear Zone, Dom Feliciano Belt, southern Brazil

Author:

Jesus Santana João Pedro de,Koester EdineiORCID,Vieira Daniel Triboli,Bastos Vivianne Andrade,Ramos Rodrigo Chaves,Porcher Carla Cristine,Bertotti Anelise L.,Cedeño Daniel Grings,Dal Olmo-Barbosa Laércio

Funder

Conselho Nacional de Desenvolvimento Científico e Tecnológico

Fundação de Amparo à Pesquisa do Estado do Rio Grande do Sul

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference74 articles.

1. Brazilian structural provinces: an introduction;Almeida;Earth Sci. Rev.,1981

2. Genesis of the two main types of peraluminous granitoids;Barbarin;Geology,1996

3. A review of the relationships between granitoid types, their origins and their geodynamic environments;Barbarin;Lithos,1999

4. The Dom Feliciano belt of Brazil and Uruguay and its foreland domain the rio de la Plata craton: framework, tectonic evolution and correlation with similar provinces of southwestern africa;Basei,2000

5. Unravelling major magmatic episodes from metamorphic sequences of the Dom Feliciano Belt central sector, southernmost Brazil–A comparative study of geochronology, elemental geochemistry, and Sr-Nd data;Battisti;Precambrian Res.,2023

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