One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The northern portion is characterized by prominent basement structures and a thick-skinned orogenic front with relief of over 2000 m with a deep level of exhumation where more than 4 km of section has been eroded. Contrastingly, the southern part is formed by mildly inverted basement structures restricted mainly to the hinterland zone, which reaches only 1500–1700 m relief. We quantify the variable contributions of two main contractional stages through the construction of three regionally balanced sections across the Andes, constrained by field and geophysical data. Extensional re-activation described for this segment in late Oligocene-early Mioc...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
International audienceNew fieldwork and tectonic analysis has been carried out along the Andean morp...
The Andes are thought to be formed through discrete contractional stages separated by periods of lit...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
This paper integrates data to summarize the evolution of the 37-39°S segment of the Andean margin fr...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The Southern Central Andes at 36°S have been recognized as an orogenic belt where contraction, accom...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The southern Central Andes recorded retroarc shortening, basin evolution, and magmatic arcmigration ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
International audienceNew fieldwork and tectonic analysis has been carried out along the Andean morp...
The Andes are thought to be formed through discrete contractional stages separated by periods of lit...
The Andean internal zone records deformation, uplift and erosion that serve as proxies of variations...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
This paper integrates data to summarize the evolution of the 37-39°S segment of the Andean margin fr...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
The Southern Central Andes at 36°S have been recognized as an orogenic belt where contraction, accom...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The southern Central Andes recorded retroarc shortening, basin evolution, and magmatic arcmigration ...
The hinterland zone of the North Patagonian Andes between 41° and 43°S constitutes a poorly explored...
The Andes between 28° and 30°S represent a transition between the Puna-Altiplano Plateau and the Fro...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
International audienceNew fieldwork and tectonic analysis has been carried out along the Andean morp...