Seismic and field-sedimentary evidence from the eastern border of the Northern Puna represent important constraints for depositional development in Andean sedimentary basin studies. The studied basin fill sequences unconformably overlay the Paleozoic Santa Victoria Group and the Cretaceous e Paleocene Salta Group. Erosive truncations, folds and faults of the Salta Group seismic sequences suggest the existence of a pre-Upper Eocene phase of deformation, which was characterized by generalized erosion and the development of a proto-depocenter. The landscape that emerged from this early stage of deformation subsequently controlled the onset of the Upper Eocene sedimentation. Cenozoic sequences are characterized by syntectonic features, such as ...
The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes t...
The Eocene-lower Oligocene Capas Rojas basin of the Cusco area is located at the northem end of the ...
The Tres Cruces basin presents an excellent record of deposits linked to the evolution of the forela...
The Quebrada de los Colorados Formation, at the north end of Calchaquí Valley in Salta Province, nor...
The stratigraphic and sedimentological characteristics of the Payogastilla Group represent important...
The Puna Plateau, adjacent Eastern Cordillera and the Sierras Pampeanas of the central Andes are lar...
Unravelling the spatiotemporal evolution of the Cenozoic Andean (Altiplano-Puna) plateau has been on...
The Quebrada de los Colorados Formation, at the north end of Calchaquí Valley in Salta Province, nor...
textThe fault-bounded Cianzo basin represents a Cenozoic intermontane depocenter between the Puna pl...
The Andean foreland basin overlaps the Cretaceous-Paleogene Salta rift basin in northwestern Argenti...
The stratigraphic and sedimentologic characteristics of Cenozoic deposits in north‐western Argentina...
The regional deformation history of the southern Puna Plateau remains poorly constrained but is key ...
The onset of deformation in the northern Andes is overprinted by subsequent stages of basin deformat...
The onset of deformation in the northern Andes is overprinted by subsequent stages of basin deformat...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes t...
The Eocene-lower Oligocene Capas Rojas basin of the Cusco area is located at the northem end of the ...
The Tres Cruces basin presents an excellent record of deposits linked to the evolution of the forela...
The Quebrada de los Colorados Formation, at the north end of Calchaquí Valley in Salta Province, nor...
The stratigraphic and sedimentological characteristics of the Payogastilla Group represent important...
The Puna Plateau, adjacent Eastern Cordillera and the Sierras Pampeanas of the central Andes are lar...
Unravelling the spatiotemporal evolution of the Cenozoic Andean (Altiplano-Puna) plateau has been on...
The Quebrada de los Colorados Formation, at the north end of Calchaquí Valley in Salta Province, nor...
textThe fault-bounded Cianzo basin represents a Cenozoic intermontane depocenter between the Puna pl...
The Andean foreland basin overlaps the Cretaceous-Paleogene Salta rift basin in northwestern Argenti...
The stratigraphic and sedimentologic characteristics of Cenozoic deposits in north‐western Argentina...
The regional deformation history of the southern Puna Plateau remains poorly constrained but is key ...
The onset of deformation in the northern Andes is overprinted by subsequent stages of basin deformat...
The onset of deformation in the northern Andes is overprinted by subsequent stages of basin deformat...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Andean Plateau of north‐western Argentina (Puna) at a mean elevation of ca. 4.2 km constitutes t...
The Eocene-lower Oligocene Capas Rojas basin of the Cusco area is located at the northem end of the ...
The Tres Cruces basin presents an excellent record of deposits linked to the evolution of the forela...