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...
Guardado en:
| Publicado: |
2016
|
|---|---|
| Materias: | |
| Acceso en línea: | https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_23174889_v46_n4_p567_DeOliveiraCarvalho http://hdl.handle.net/20.500.12110/paper_23174889_v46_n4_p567_DeOliveiraCarvalho |
| Aporte de: |
Ejemplares similares
-
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
por: De Oliveira Carvalho, M., et al. -
Thick-skinned and thin-skinned thrusting in the La Ramada fold and thrust belt: Crustal evolution of the High Andes of San Juan, Argentina (32°SL)
por: Cristallini, E.O., et al. -
Thick-skinned and thin-skinned thrusting in the La Ramada fold and thrust belt: Crustal evolution of the High Andes of San Juan, Argentina (32°SL)
Publicado: (2000) -
Temporal and spatial relationships of thick- and thin-skinned deformation: A case study from the Malargüe fold-and-thrust belt, southern Central Andes
por: Giambiagi, L., et al. -
Temporal and spatial relationships of thick- and thin-skinned deformation: A case study from the Malargüe fold-and-thrust belt, southern Central Andes
Publicado: (2008)