The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tectonic inversion of extensional structures of Early to Middle Jurassic age in the Main Andes to Oligocene in the Precordilleran region. These have acted during two distinctive orogenic stages, first in late Early Cretaceous and later in Miocene times Late Oligocene extension separates these two contractional periods and is recorded by half-grabens developed in the retroarc region. The last contractional stage coexists with an eastward foreland expansion of the late Miocene arc whose roots are presently exposed as minor granitic stocks and volcanic piles subordinately in the Main Andes, east of the present arc. As a consequence of this orogenic ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Ma...
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...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which are record...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The Patagonian Andes represents a unique natural laboratory to study surface deformation in relation...
The distribution and timing of the deformation for the North Patagonian broken foreland is nowadays ...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Ma...
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...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
Miocene sedimentary successions of the Ñirihuau and Collón Cura formations east of the El Maitén Bel...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
The intraplate fault-block mountains and intermontane deposits of the Gastre Basin, which are record...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The Patagonian Andes represents a unique natural laboratory to study surface deformation in relation...
The distribution and timing of the deformation for the North Patagonian broken foreland is nowadays ...
One of the main morphological changes along the Southern Central Andes occurs from 36° to 39°S. The ...
The Catán Lil Basin is an intermontane basin developed on the wedge top of the Miocene North Patagon...
The structure and tectonics of the retro-arc area of the Andes between 38°30' and 40°S remains poorl...
The tectonic regime associated with the Oligo-Miocene Cura-Mallín Formationand equivalents in the Ma...