Stratigraphy and structure of the Argentine Central Andes between 30°and 31°S latitude

In a cross-section through the Argentine central Andes, two large groups of rocks can be distinguished: a Gondwanic (Paleozoic) basement, and an Andean cover. The basement is constituted by marine sedimentary units, intruded by Upper Paleozoic granitoid rocks. The most important Gondwanic structures...

Descripción completa

Guardado en:

Detalles Bibliográficos
Autores principales:	Rodríguez Fernández, L.R., Heredia, N., Espina, R.G., Cegarra, M.I.
Formato:	JOUR
Materias:	Andean cordillera Andean orogeny Gondwanic orogeny Tectonic inversion Gondwana orogeny stratigraphy tectonic evolution South America
Acceso en línea:	http://hdl.handle.net/20.500.12110/paper_05677505_v32_n1-2_p51_RodriguezFernandez
Aporte de:	Biblioteca Digital - Facultad de Ciencias Exactas y Naturales (UBA) de Universidad de Buenos Aires

Ejemplares similares

Stratigraphy and structure of the Argentine Central Andes between 30°and 31°S latitude
Publicado: (1997)

The tertiary units of the Rodeo-Iglesia Basin: Validity and correlation of the formational units
Publicado: (2001)

The tertiary units of the Rodeo-Iglesia Basin: Validity and correlation of the formational units
por: Gagliardo, M.L., et al.

Cenozoic tectonic evolution of the Alto Tunuyán foreland basin above the transition zone between the flat and normal subduction segment (33°30′-34°S), western Argentina
Publicado: (2001)

Cenozoic tectonic evolution of the Alto Tunuyán foreland basin above the transition zone between the flat and normal subduction segment (33°30′-34°S), western Argentina
por: Giambiagi, L.B., et al.

Tectono-stratigraphic evolution of the Andean Orogen between 31 and 37°S (Chile and Western Argentina)
por: Charrier, R., et al.

Tectono-stratigraphic evolution of the Andean Orogen between 31 and 37°S (Chile and Western Argentina)
Publicado: (2015)

The subhorizontal subduction segment in the Argentinian-Chilean Central Andes
por: Ramos, Victor Alberto
Publicado: (1997)

The subhorizontal subduction segment in the Argentinian-Chilean Central Andes
por: Ramos, V.A.

Stratigraphy of the Neogene, Paleogene and Mesozoic successions of the Santo Domingo and El Peñón creeks (Northern Precordillera of La Rioja)
por: Limarino, Carlos Oscar, et al.
Publicado: (2016)

Stratigraphy of the Neogene, Paleogene and Mesozoic successions of the Santo Domingo and El Peñón creeks (Northern Precordillera of La Rioja)
por: Limarino, C.O., et al.

Review of the Cambrian Pampean orogeny of Argentina; a displaced orogen formerly attached to the Saldania Belt of South Africa?
por: Casquet, César, et al.
Publicado: (2018)

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

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

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.

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)

An Andean tectonic cycle: From crustal thickening to extension in a thin crust (34°-37°SL)
Publicado: (2014)

An Andean tectonic cycle: From crustal thickening to extension in a thin crust (34°-37°SL)
por: Ramos, V.A., et al.

Late Cenozoic contractional evolution of the current arc-volcanic region along the southern Central Andes (35°20'S)
por: Naipauer, Maximiliano
Publicado: (2015)

Late Cenozoic contractional evolution of the current arc-volcanic region along the southern Central Andes (35°20'S)
por: Tapia, F., et al.

The andean movements of groeber and the tectonic evolution of the southern central Andes
por: Mescua, José Francisco, et al.
Publicado: (2017)

The andean movements of groeber and the tectonic evolution of the southern central Andes
por: Mescua, J.F., et al.

Emplacement conditions and exhumation of the Varvarco Tonalite and associated plutons from the Cordillera del Viento, Southern Central Andes
por: Assis, Omar, et al.
Publicado: (info)

Paleomagnetic evidence of the brittle deformation of the Central Patagonian Batholith at Gastre area (Chubut Province, Argentina)
por: Ruiz González, Víctor, et al.
Publicado: (2020)

Tertiary succesion of the Los Pozuelos creek (Vinchina Basin): Its stratigraphic and paleogeographic importance for the Andean foreland
Publicado: (2013)

Tertiary succesion of the Los Pozuelos creek (Vinchina Basin): Its stratigraphic and paleogeographic importance for the Andean foreland
por: Ciccioli, P.L., et al.

Metamorphic ages of low-grade units in the central region of Famatina: The signature of the Ocloyic Orogeny (Ordovician)
por: Collo, G., et al.

Metamorphic ages of low-grade units in the central region of Famatina: The signature of the Ocloyic Orogeny (Ordovician)
Publicado: (2008)

Low-grade metamorphism of cambro-ordovician successions in the famatina belt, southern-central andes: Burial-inversion history linked to the evolution of the proto-andean gondwana margin
por: Do Campo, Margarita Diana
Publicado: (2011)

Low-grade metamorphism of cambro-ordovician successions in the famatina belt, southern-central andes: Burial-inversion history linked to the evolution of the proto-andean gondwana margin
por: Collo, G., et al.

Tectonic evolution of the North Patagonian Andes (41°–44° S) through recognition of syntectonic strata
por: Folguera, Andrés, et al.
Publicado: (2016)

Tectonic evolution of the North Patagonian Andes (41°–44° S) through recognition of syntectonic strata
por: Echaurren, A., et al.

Tectonic characterization of the mesoscopic kinking from the Sierras Australes of Buenos Aires
por: Rossello, Eduardo Antonio, et al.
Publicado: (1992)

Tectonic characterization of the mesoscopic kinking from the Sierras Australes of Buenos Aires
por: Rossello, E.A., et al.

Numerical modeling for the upper crustal deformation in the Southern Andes
por: Quinteros, Javier, et al.
Publicado: (2005)

Numerical modeling for the upper crustal deformation in the Southern Andes
por: Quinteros, J., et al.
Publicado: (2005)

Numerical modeling for the upper crustal deformation in the Southern Andes
por: Quinteros, J., et al.

Numerical modeling for the upper crustal deformation in the Southern Andes
por: Quinteros, J., et al.
Publicado: (2005)

Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana
Publicado: (2019)

Evolution of the Major Gercino Shear Zone in the Dom Feliciano Belt, South Brazil, and implications for the assembly of southwestern Gondwana
por: Hueck, M., et al.