This chapter focuses on the structural styles of the Villa Unión-San Isidro basement-involved fold and thrust belt in the northern Ischigualasto-Villa Unión Basin of the western Sierras Pampeanas, La Rioja Province, Argentina. The region is situated within the Pampean flat-slab subduction segment (28°–32°30′S) of the Central Andes, and it records the Neogene phase of the Andean orogeny through many basement-involved structures, such as analyzed in this chapter. Detailed seismic interpretation of two poststack time migrated seismic reflection profiles indicates the presence of three WSW–ENE to SW–NE-trending and SE-vergent reverse and thrust blind faults that generate fault-bend folds and fault-propagation folds. In addition to these structu...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
In this work we study the evolution of one particular segment of the Southern Central Andes, the nor...
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volca...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The deformation front of the Neuquén fold and thrust belt (~37°30′S) comprises kilometer-scale basem...
The study area is located within the Central Andes, a complex region composed of different structura...
The study area is located within the Central Andes, a complex region composed of different structura...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
Andean orogenesis is expressed in the diverse deformational records of crustal structures and sedime...
This paper describes Late Paleozoic Gondwanan and Late Cretaceous to Early Cenozoic Andean structure...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
In this work we study the evolution of one particular segment of the Southern Central Andes, the nor...
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volca...
In the southern Central Andes, the Andean foreland was deformed due to Neogene shallowing of the Naz...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
The Malargüe fold-and-thrust belt is a thick-skinned belt developed in Miocene-Pliocene times during...
The Chos Malal fold and thrust belt is a thick-skinned mountain belt that deformed the Mesozoic de...
The deformation front of the Neuquén fold and thrust belt (~37°30′S) comprises kilometer-scale basem...
The study area is located within the Central Andes, a complex region composed of different structura...
The study area is located within the Central Andes, a complex region composed of different structura...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
Andean orogenesis is expressed in the diverse deformational records of crustal structures and sedime...
This paper describes Late Paleozoic Gondwanan and Late Cretaceous to Early Cenozoic Andean structure...
Superposed structural fabrics in the easternmost Fuegian Andes reveal two distinct, non-coaxial defo...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
In this work we study the evolution of one particular segment of the Southern Central Andes, the nor...
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volca...