This review synthesizes the tectonomagmatic evolution of the southern Central andNorthern Patagonian Andes between 35°30?S to 48°S with the aim to spotlight earlycontractional phases on Andean orogenic building and to analyze their potential drivingprocesses. We examine early tectonic stages of the different fold and thrust belts that composethis Andean segment. Additionally, we study the magmatic arc behavior from a regionalperspective as an indicator of potential past subduction configurations during critical tectonicstages of orogenic construction. This revision proposes the existence of a continuous large-scaleflat subduction with a similar size to the present-largest flat-slab setting on earth. This particularprocess would have initiat...
We present field and seismic evidence for the existence of Coniacian–Campanian syntectonic angular u...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
In active continental margins, mountain building processes have been classically referred to as Ande...
The kinematics of the Farallon-Phoenix-South America triple junction during the Cretaceous and Paleo...
After a Late Cretaceous to Paleocene stage of mountain building, the North Patagonian Andes were ext...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
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...
The Neuquén Group is an Upper Cretaceous continental sedimentary unit exhumed during the latest Mioc...
The Central Patagonia is characterized by prominent continental deposits that belong to the Cretaceo...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
This paper analyzes the style, distribution, mechanics, and timing of deformation of the Andean retr...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
We present field and seismic evidence for the existence of Coniacian–Campanian syntectonic angular u...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
In active continental margins, mountain building processes have been classically referred to as Ande...
The kinematics of the Farallon-Phoenix-South America triple junction during the Cretaceous and Paleo...
After a Late Cretaceous to Paleocene stage of mountain building, the North Patagonian Andes were ext...
The North Patagonian fold-thrust belt (41°–44° S) is characterized by a low topography, reduced crus...
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...
The Neuquén Group is an Upper Cretaceous continental sedimentary unit exhumed during the latest Mioc...
The Central Patagonia is characterized by prominent continental deposits that belong to the Cretaceo...
The transition zone from the Southern Central to the North PatagonianAndes is characterized by a low...
In the last decades an important amount of studies have dealt with the Patagonian orogen. However, a...
The Northern Patagonian Andes have been constructed through multiple mechanisms that range from tect...
This paper analyzes the style, distribution, mechanics, and timing of deformation of the Andean retr...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
We present field and seismic evidence for the existence of Coniacian–Campanian syntectonic angular u...
In this classic segment, many tectonic processes, like flat-subduction, terrane accretion and steepe...
In active continental margins, mountain building processes have been classically referred to as Ande...