Southern Patagonian plateau basalts and deformation: Backarc testimony of ridge collisions

The distribution and volume of Tertiary Patagonian plateau basalts and the evolution of the Patagonian fold and thrust belt between 46° and 49°S appear to be closely tied with ridge-trench interactions along the continental margin to the west. Eocene plateau basalts south of 43°S are associated with...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Ramos, V.A., Kay, S.M.
Formato:	JOUR
Materias:	basalt fold and thrust belt mantle source ridge/trench interaction slab window Tertiary Argentina, Patagonia
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_00401951_v205_n1-3_p261_Ramos
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

Ejemplares similares

Southern Patagonian plateau basalts and deformation: Backarc testimony of ridge collisions
Publicado: (1992)

Neogene Patagonian plateau lavas: Continental magmas associated with ridge collision at the Chile Triple Junction
por: Gorring, M.L., et al.

Neogene Patagonian plateau lavas: Continental magmas associated with ridge collision at the Chile Triple Junction
Publicado: (1997)

Plume overriding triggers shallow subduction and orogeny in the southern Central Andes
Publicado: (2017)

Plume overriding triggers shallow subduction and orogeny in the southern Central Andes
por: Gianni, G.M., et al.

The origin of the Loncopué Trough in the retroarc of the Southern Central Andes from field, geophysical and geochemical data
por: Rojas Vera, E.A., et al.

The origin of the Loncopué Trough in the retroarc of the Southern Central Andes from field, geophysical and geochemical data
Publicado: (2014)

New evidence of the importance of faulting in the structure of the Sierras Australes de la Provincia de Buenos Aires
por: Tomezzoli, Renata Nela
Publicado: (1998)

New evidence of the importance of faulting in the structure of the Sierras Australes de la Provincia de Buenos Aires
por: Tomezzoli, R.N.
Publicado: (1998)

New evidence of the importance of faulting in the structure of the Sierras Australes de la Provincia de Buenos Aires
por: Tomezzoli, R.N.

New evidence of the importance of faulting in the structure of the Sierras Australes de la Provincia de Buenos Aires
por: Tomezzoli, R.N.
Publicado: (1998)

Andean deformation at the cordón del Hielo Azul, El Bolsón, Río Negro (Argentina). Implications for the tectonic evolution of the north Patagonian Andes
por: Tobal, J.E., et al.

Palaeomagnetic data from the Precordillera fold and thrust belt constraining Neogene foreland evolution of the Pampean flat-slab segment (Central Andes, Argentina)
por: Japas, Maria Silvia, et al.
Publicado: (2016)

Palaeomagnetic data from the Precordillera fold and thrust belt constraining Neogene foreland evolution of the Pampean flat-slab segment (Central Andes, Argentina)
por: Japas, M.S., et al.

Reactivation of Paleozoic structures during Cenozoic deformation in the Cordón del Plata and Southern Precordillera ranges (Mendoza, Argentina)
Publicado: (2014)

Reactivation of Paleozoic structures during Cenozoic deformation in the Cordón del Plata and Southern Precordillera ranges (Mendoza, Argentina)
por: Giambiagi, L., et al.

Andean deformation at the cordón del Hielo Azul, El Bolsón, Río Negro (Argentina). Implications for the tectonic evolution of the north Patagonian Andes
Publicado: (2012)

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)

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.

The Farallon-Aluk ridge collision with South America: Implications for the geochemical changes of slab window magmas from fore- to back-arc
por: Aragón, Eugenio, et al.
Publicado: (2013)

Geochemistry of mafic Paleocene volcanic rocks in the Valle del Cura region: Implications for the petrogenesis of primary mantle-derived melts over the Pampean flat-slab
por: Litvak, Vanesa Dafne, et al.
Publicado: (2010)

Geochemistry of mafic Paleocene volcanic rocks in the Valle del Cura region: Implications for the petrogenesis of primary mantle-derived melts over the Pampean flat-slab
por: Litvak, V.D., et al.

Structural evolution of the Andes in a transitional zone between flat and normal subduction (33°30′-33°45′S), Argentina and Chile
por: Giambiagi, L.B., et al.

Seismic ridge subduction and topography: Foreland deformation in the Patagonian Andes
por: Ramos, V.A.

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.

Evolución estructural mesozoica para el valle del río Atuel entre el Cerro Sosneado y la Cuchilla de la Tristeza, Mendoza, Argentina
por: Fortunatti, Natalia Beatriz
Publicado: (2010)

Mechanisms and deformational stages at the eastern Andean front (36°S, Argentina)
por: Álvarez Cerimedo, J., et al.

Middle to late Miocene extensional collapse of the North Patagonian Andes (41°30′-42°S)
por: Tobal, J.E., et al.

Crustal collapse in the Andean backarc since 2 Ma: Tromen volcanic plateau, Southern Central Andes (36°40′-37°30′S)
por: Folguera, A., et al.

Structural evolution of the Andes in a transitional zone between flat and normal subduction (33°30′-33°45′S), Argentina and Chile
Publicado: (2002)

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
Publicado: (2016)

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.

Structure and development of the Andean system between 36° and 39°S
por: Rojas Vera, E.A., et al.

Middle to late Miocene extensional collapse of the North Patagonian Andes (41°30′-42°S)
Publicado: (2015)

Mechanisms and deformational stages at the eastern Andean front (36°S, Argentina)
Publicado: (2013)

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)

Seismic ridge subduction and topography: Foreland deformation in the Patagonian Andes
Publicado: (2005)

Structure and development of the Andean system between 36° and 39°S
Publicado: (2014)

Influence of pre-Andean history over cenozoic foreland deformation: Structural styles in the malargüe fold-and-thrust belt at 35°S, andes of Argentina
por: Mescua, J.F., et al.

Crustal collapse in the Andean backarc since 2 Ma: Tromen volcanic plateau, Southern Central Andes (36°40′-37°30′S)
por: Folguera, Andrés, et al.
Publicado: (2008)