The thrust contact between the Canastra and Vazante groups in the Southern Brasília Belt: Structural evolution, white mica crystallinity and implications for the Brasiliano orogeny
Two regional thrust-sheets of Neoproterozoic metasedimentary rocks occur in the Southern Brasilia Belt, northwest Minas Gerais. The lower one comprises the Vazante Group, that is formed in the studied area, from base to top, by the Serra do Garrote (metapelites interlayered with carbonaceous phyllit...
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| Autores principales: | De Oliveira Carvalho, M., De Morisson Valeriano, C., González, P.A.A., Oliveira, G.D., Impiccini, A. |
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| Formato: | JOUR |
| Materias: | |
| Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_23174889_v46_n4_p567_DeOliveiraCarvalho |
| Aporte de: |
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