The drainage pattern on the western piedmont of the Sierra de La Cantera is divergent, typical of alluvial fans and showing anomalies that are directly related to the trace of La Cantera thrust. In previous studies, two types of anomalies were identified: upstream of the fault scarp, rivers have a broom-shaped pattern, while downstream – in the hanging block – streams become denser, more sinuous and incised. In this contribution, these morphotectonic aspects were analyzed in detail, making direct and indirect analysis to quantify the relationship between these anomalies and the faults affecting alluvial fans. In addition, the influence of neotectonic activity on smaller water course patterns in the alluvial fan areas was investigated in ord...
The Central and Eastern Precordillera form oppositely verging thrust systems on the western and east...
Longitudinal profiles were analyzed in the rivers of the central sector of the Araucaria Plateau, ai...
This investigation reveals the relative susceptibility of the landscape to surface deformation by me...
Between 31°45'-32°15' S, the western piedmont of the Ansilta block in the Precordillera of Argentina...
Analysis of several morphotectonic tools (longitudinal river profiles, knickpoints, swath profiles, ...
El área de estudio corresponde al sector norte del sobrecorrimiento La Cantera, ubicado a 56 km al n...
The La Cantera Fault System (LCFS) is the most active Quaternary structure in the Central Precordill...
Recently, geomorphometric properties of river networks and catchments have been described and applie...
Se estudia la morfología y dinámica del abanico aluvial del río Salado del Norte, localizado en la r...
Morphometric analysis of the Tajo drainage network using a DEM was carried out in order to determine...
Northern Apennines is tectonically an active fold and thrust belt. Digital Elevation Model (DEM) bas...
The San Juan River, located in San Juan Province (Argentina), crosses the Precordillera and other ge...
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de ...
The tectonically active broken foreland of NW Argentina is a recent analog of the eastern margin of ...
En la ladera occidental del sector norte de la sierra Chica de Zonda, Precordillera Oriental, provin...
The Central and Eastern Precordillera form oppositely verging thrust systems on the western and east...
Longitudinal profiles were analyzed in the rivers of the central sector of the Araucaria Plateau, ai...
This investigation reveals the relative susceptibility of the landscape to surface deformation by me...
Between 31°45'-32°15' S, the western piedmont of the Ansilta block in the Precordillera of Argentina...
Analysis of several morphotectonic tools (longitudinal river profiles, knickpoints, swath profiles, ...
El área de estudio corresponde al sector norte del sobrecorrimiento La Cantera, ubicado a 56 km al n...
The La Cantera Fault System (LCFS) is the most active Quaternary structure in the Central Precordill...
Recently, geomorphometric properties of river networks and catchments have been described and applie...
Se estudia la morfología y dinámica del abanico aluvial del río Salado del Norte, localizado en la r...
Morphometric analysis of the Tajo drainage network using a DEM was carried out in order to determine...
Northern Apennines is tectonically an active fold and thrust belt. Digital Elevation Model (DEM) bas...
The San Juan River, located in San Juan Province (Argentina), crosses the Precordillera and other ge...
A geomorphologic and morphometric analysis was performed to determine the characteristics of the de ...
The tectonically active broken foreland of NW Argentina is a recent analog of the eastern margin of ...
En la ladera occidental del sector norte de la sierra Chica de Zonda, Precordillera Oriental, provin...
The Central and Eastern Precordillera form oppositely verging thrust systems on the western and east...
Longitudinal profiles were analyzed in the rivers of the central sector of the Araucaria Plateau, ai...
This investigation reveals the relative susceptibility of the landscape to surface deformation by me...