The analysis of mid-scale distributive fluvial systems (DFS) provides an opportunity to study fluvial depositional patterns in sedimentary basins in a manner similar to megafans, but under the more homogeneous external conditions that control small alluvial fans from the source area to the depositional area. Four mid-scale Quaternary DFS and the areas of their drainage basins were analysed with the aim of understanding and predicting the mechanism and magnitude of fluvial fan deposition. These DFS were located in the Gastre Basin, Argentina, an endorheic basin that has evolved during the Quaternary under relatively uniform climatic and tectonic conditions. Using a geomorphological and sedimentological approach, the measured areas of the DFS...
An integrated stratigraphic, sedimentological and petrophysical analysis is presented to document th...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...
Evaluating the role of tectonics and climate as possible triggering mechanisms of landscape reconfig...
The Hauterivian Avilé Member of the Agrio Formation constitutes a non marine lowstand wedge dominate...
The seaward end of modern rivers is marked by the fluvial to marine transition zone (FMTZ), which is...
The Cretaceous Chubut Group in the Golfo San Jorge Basin (Patagonia, Argentina) comprises up to 6000...
Investigating the controls of fluvial erosion and how these controls are recorded in topography is k...
The Kimmeridgian Quebrada del Sapo Formation in the southernmost Neuquén Basin in Argentina represen...
The seaward end of modern rivers is characterized by the interactions of marine and fluvial processe...
Sediment discharge events in the lower basin of the Chubut River (Patagonia, Argentina) associated w...
The morphometric characteristics of the Moneta river basin are compared to those of the Avilés river...
In terminal fluvial‐fan systems, characteristic proximal to distal variations in sedimentary archite...
One of the most challenging aspects when analyzing the stratigraphic architectures ofancient basins ...
In terminal fluvial‐fan systems, characteristic proximal to distal variations in sedimentary archite...
An integrated stratigraphic, sedimentological and petrophysical analysis is presented to document th...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...
Evaluating the role of tectonics and climate as possible triggering mechanisms of landscape reconfig...
The Hauterivian Avilé Member of the Agrio Formation constitutes a non marine lowstand wedge dominate...
The seaward end of modern rivers is marked by the fluvial to marine transition zone (FMTZ), which is...
The Cretaceous Chubut Group in the Golfo San Jorge Basin (Patagonia, Argentina) comprises up to 6000...
Investigating the controls of fluvial erosion and how these controls are recorded in topography is k...
The Kimmeridgian Quebrada del Sapo Formation in the southernmost Neuquén Basin in Argentina represen...
The seaward end of modern rivers is characterized by the interactions of marine and fluvial processe...
Sediment discharge events in the lower basin of the Chubut River (Patagonia, Argentina) associated w...
The morphometric characteristics of the Moneta river basin are compared to those of the Avilés river...
In terminal fluvial‐fan systems, characteristic proximal to distal variations in sedimentary archite...
One of the most challenging aspects when analyzing the stratigraphic architectures ofancient basins ...
In terminal fluvial‐fan systems, characteristic proximal to distal variations in sedimentary archite...
An integrated stratigraphic, sedimentological and petrophysical analysis is presented to document th...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...
Les « distributive fluvial systems »(DFS) sont d'importants éléments géomorphologiques pouvant domin...