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Petrographic and mineralogical characterization of magmatic-hydrothermal breccia at Itatiaia alkaline complex, Rio de Janeiro state: occurrences of fluorite and REE minerals
The meso-cenozoic alkaline magmatism in Rio de Janeiro is represented by several plutonic/volcanic bodies, which occurred on W-E fracture and lineaments zones associated with the development of the Southeastern Brazilian Rift. One of main occurrences of those rocks is the Itatiaia Alkaline Complex (...
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| Main Authors: | , , , |
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| Formato: | Online |
| Idioma: | por |
| Publicado em: |
Universidade Federal do Rio de Janeiro
2014
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| Acesso em linha: | https://revistas.ufrj.br/index.php/aigeo/article/view/6970 |
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