Between 31°45'-32°15' S, the western piedmont of the Ansilta block in the Precordillera of Argentina has been uplifted in Quaternary times through folds, blind faults and faulted blocks that form discrete and evident areas of neotectonic deformation (structural highs). In between, subtle tectonic perturbations of the fluvial landforms (drainage anomalies), such as diverted and entrenched streams, asymmetric basins, incision anomalies, convex-upward longitudinal stream profiles, dammed rivers and broom-shaped patterns allow the recognition of areas of incipient deformation. We combined the analyses of both the structural highs and the drainage anomalies areas to investigate the role of the latest as an expression of soft-linkage areas in fau...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
Analysis of several morphotectonic tools (longitudinal river profiles, knickpoints, swath profiles, ...
The drainage pattern on the western piedmont of the Sierra de La Cantera is divergent, typical of al...
The tectonically active broken foreland of NW Argentina is a recent analog of the eastern margin of ...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
Uplift in the broken Andean foreland of the Argentine Santa Bárbara System (SBS) is associated with ...
The evolution of the drainage pattern of the eastern Andes has proven to be a valuable indicator of ...
Curved traces are recurrent features of structural map-view patterns on different fold and thrust be...
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volca...
The Central and Eastern Precordillera form oppositely verging thrust systems on the western and east...
The intermontane Quebrada de Humahuaca Basin (Humahuaca Basin) in the Eastern Cordillera of the sout...
The NNW-trending Las Peñas Thrust System is one of the key structures along the Andean orogenic fron...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...
Analysis of several morphotectonic tools (longitudinal river profiles, knickpoints, swath profiles, ...
The drainage pattern on the western piedmont of the Sierra de La Cantera is divergent, typical of al...
The tectonically active broken foreland of NW Argentina is a recent analog of the eastern margin of ...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
Uplift in the broken Andean foreland of the Argentine Santa Bárbara System (SBS) is associated with ...
The evolution of the drainage pattern of the eastern Andes has proven to be a valuable indicator of ...
Curved traces are recurrent features of structural map-view patterns on different fold and thrust be...
The Nevados del Famatina, located in northwestern Argentina (Fig. 1), is one of the higher non-volca...
The Central and Eastern Precordillera form oppositely verging thrust systems on the western and east...
The intermontane Quebrada de Humahuaca Basin (Humahuaca Basin) in the Eastern Cordillera of the sout...
The NNW-trending Las Peñas Thrust System is one of the key structures along the Andean orogenic fron...
To improve the knowledge about the Quaternary tectonic landforms, their potential level of activity,...
A neotectonic study at the transitional segment between the Central and North Patagonian Andes, in t...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
International audienceThe southern central Andes foothills are made of imbricate thick- and thin-ski...