The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geophysical data in order to decipher the deformationalprocesses that acted through time and relate them to basin formation. Fieldobservations and seismic reflection profiles reveal the shallow structure of theretroarc area where contractional structures, associated with Oligocene to earlyMiocene inverted extensional sections, are partially onlapped by early to lateMiocene synorogenic deposits. From the construction of five structural cross sections along the retroarc area between 40° and 43° 30′S, constrained by surface, gravity, and seismic data, a shortening gradient is observed along Andean strike. The highest shortening of 18.7 km (15.34 %)...
The Patagonian Andes represents a unique natural laboratory to study surface deformation in relation...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
After a Late Cretaceous to Paleocene stage of mountain building, the North Patagonian Andes were ext...
The Andes in northern Patagonia are mainly formed by Mesozoic magmatic units: the mostly Jurassic-Cr...
The Patagonian Andes represents a unique natural laboratory to study surface deformation in relation...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
After a Late Cretaceous to Paleocene stage of mountain building, the North Patagonian Andes were ext...
The Andes in northern Patagonia are mainly formed by Mesozoic magmatic units: the mostly Jurassic-Cr...
The Patagonian Andes represents a unique natural laboratory to study surface deformation in relation...
This chapter is focused on the tectonic evolution of the North PatagonianAndes comprised between 38°...
The Central Andes are the product of contractional deformation related to subduction of the Nazca pl...