4   Artículos

 
en línea
Fernando Lebinson,Martín Turienzo,Natalia Sánchez,Vanesa Araujo,María Celeste D?Annunzio,Luis Dimieri     Pág. 249 - 273
The Agrio fold and thrust belt is a thick-skinned orogenic belt developed since Late Cretaceous in response to the convergence between the Nazca and South American plates. The integration of new structural field data and seismic line interpretation allow... ver más
Revista: Andean Geology    Formato: Electrónico

 
en línea
O. Adrian Pfiffner and Laura Gonzalez    
Based on the structural style and physiographic criteria, the Central Andes of Peru can be divided into segments running parallel to the Pacific coast. The westernmost segment, the Coastal Belt, consists of a Late Jurassic?Cretaceous volcanic arc sequenc... ver más
Revista: Geosciences    Formato: Electrónico

 
en línea
Lucia Sagripanti,German Bottesi,Diego Kietzmann,Andres Folguera,Victor Ramos     Pág. 201 - 219
The orogenic front at 37ºS has been mainly formed through at least two contraccional stages, as inferred from the exhumed major angular unconformities at the Late Eocene and the Late Miocene times respectively. A Late Cretaceous event is restricted to th... ver más
Revista: Andean Geology    Formato: Electrónico

 
en línea
Darío L. Orts,Andrés Folguera,Mario Giménez,Víctor Ramos     Pág. 220 - 241
The Southern Central Andes at 36ºS have been recognized as an orogenic belt where contraction, accommodatedmainly by basement structures, is associated with the inversion of a Late Triassic-Early Jurassic extensionaldetachment. Based on a structural cros... ver más
Revista: Andean Geology    Formato: Electrónico

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