Quaternary deformations described in the retro-arc region at the latitudes of the Neuquén Basin can be divided into two main groups: a northern group characterized by Quaternary deformation zones concentrated near the main topographic breaks of different morphostructural systems, and a second group located in the southern Neuquén Basin distinguished by disconnected, sparced and noncontinuous Quaternary deformational zones. In the northern Neuquén Basin, evidence of active deformation is associated with the Frontal Cordillera (33°–34° S); while in the foreland area, young deformations concentrate in the San Rafael Block. In the southern Neuquén Basin, a western deformational belt constitutes the continuation to the north of an intra-arc faul...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
Back-arcs are hot regions of enduring weakness in the hinterland of subduction zones that are common...
Understanding the geometry and kinematics of the major structures of an orogen is important to eluci...
Quaternary deformation in the Southern Central Andes between 36° and 38°S is disconnected, noncontin...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
The Neuquén Embayment, which developed along the eastern foothills of thesouthern Central Andes, has...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
Estudios recientes focalizados en las vecindades del volcán Tromen, en el norte de la provincia de N...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
The Andes of Neuquén (36°- 38°SL) have distinctive characteristics within the Central Andes inherite...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The mechanisms and the timing of the building of the Neuquén Andes in the southern central Andes of ...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
Back-arcs are hot regions of enduring weakness in the hinterland of subduction zones that are common...
Understanding the geometry and kinematics of the major structures of an orogen is important to eluci...
Quaternary deformation in the Southern Central Andes between 36° and 38°S is disconnected, noncontin...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
The Neuquén Embayment, which developed along the eastern foothills of thesouthern Central Andes, has...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
Estudios recientes focalizados en las vecindades del volcán Tromen, en el norte de la provincia de N...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
The Andes of Neuquén (36°- 38°SL) have distinctive characteristics within the Central Andes inherite...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The mechanisms and the timing of the building of the Neuquén Andes in the southern central Andes of ...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
Back-arcs are hot regions of enduring weakness in the hinterland of subduction zones that are common...
Understanding the geometry and kinematics of the major structures of an orogen is important to eluci...