This paper integrates data to summarize the evolution of the 37-39°S segment of the Andean margin from the Miocene to Present. The western Neuquén Andes represent a transitional segment between the high, broad Central Andes and the low, narrow Patagonian Andes. The Main Cordillera integrates a ~28-11 Ma volcanic-sedimentary extensional basin, inverted between 11-6 Ma. Since 6 Ma, extension and transtension dominated the area. South of 38°S, deformation concentrated along the intra-arc Liquiñe-Ofqui fault zone, a crustal-scale dextral strike-slip system accommodating part of the margin-parallel component of oblique subduction. Volcanism is strongly controlled by the structures of this fault zone. We differentiate four main tectonic phases: (...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Andes of Neuquén (36°- 38°SL) have distinctive characteristics within the Central Andes inherite...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
We describe the Miocene–Quaternary geological–structural evolution of the region between the Salar d...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
International audienceNew fieldwork and tectonic analysis has been carried out along the Andean morp...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The fold and thrust belt of the Neuquén Andes between 37° and 37°30´S can be divided into two sector...
We describe the Miocene-Quaternary geological-structural evolution of the region between the Salar d...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Andes of Neuquén (36°- 38°SL) have distinctive characteristics within the Central Andes inherite...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
We describe the Miocene–Quaternary geological–structural evolution of the region between the Salar d...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
International audienceNew fieldwork and tectonic analysis has been carried out along the Andean morp...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The fold and thrust belt of the Neuquén Andes between 37° and 37°30´S can be divided into two sector...
We describe the Miocene-Quaternary geological-structural evolution of the region between the Salar d...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The evolution of Neogene Central Andes is characterized by the eastward propagation of deformation f...