Structural evolution of the transition zone between the Aconcagua and Malargûe fold and thrust belts, province of Mendoza
In this work we describe briefly the stratigraphy and the structure of the Andes in the transition zone between the Aconcagua and Malargüe fold and thrust belts. The outcrops are a Permotriasic volcanic acid basement, Mesozoic sediments of the Cuenca Neuquina and Neogene volcanic rocks and continent...
Guardado en:
Autores principales: | Broens, S., Pereira, D.M. |
---|---|
Formato: | JOUR |
Materias: | |
Acceso en línea: | http://hdl.handle.net/20.500.12110/paper_00044822_v60_n4_p685_Broens |
Aporte de: |
Ejemplares similares
-
Structural evolution of the transition zone between the Aconcagua and Malargûe fold and thrust belts, province of Mendoza
Publicado: (2005) -
The control of pre-existing extensional structures on the evolution of the southern sector of the Aconcagua fold and thrust belt, southern Andes
Publicado: (2003) -
The control of pre-existing extensional structures on the evolution of the southern sector of the Aconcagua fold and thrust belt, southern Andes
por: Giambiagi, L.B., et al. -
Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
Publicado: (2005) -
Lnfluence of the Triassic-Jurassic rift structures on the deformation style of the Aconcagua and Maragüe fold and thrust belts, Mendoza
por: Giambiagi, L., et al.