A high-resolution geophysical study was carried out in a region of the retroarc of the Patagonian Andes located on the western slope of the Sierra de El Maitén. This structure is characterized by an imbricated west-vergent fault system developed in the orogenic front area of the North Patagonian Andes that has uplifted. Oligocene volcanic rocks (Ventana Formation) affect Miocene to Quaternary sediments. Even though neotectonic fault scarps are affecting Quaternary deposits in the foothills of this range, no direct observation of slip in Quaternary strata was determined. The main objective of this study is to determine geometry of recognized neotectonic structures, characterizing them by variations in magnetic susceptibility, density, and p-...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
The Guacha Corral shear zone (GCSZ) is represented by mylonites that were developed under amphibolit...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
A high-resolution superficial geophysical study was carried out in an area of the retroarc region of...
The city of San Juan, in the Central-Western region of Argentina, has been the target of very destru...
Research for evaluation of geologic hazards involving earthquakes and volcanic eruptions in southern...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
This chapter focuses on the neotectonics of Argentine–Chilean Patagonia and overviews the active tec...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
Twenty-five new long-period magnetotelluric sites near 31.5°S were collected in a west–east profile....
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calcha...
The eastern Sierras Pampeanas (ESP) are the easternmost expression of a series of foreland uplifts i...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
The Guacha Corral shear zone (GCSZ) is represented by mylonites that were developed under amphibolit...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...
A high-resolution superficial geophysical study was carried out in an area of the retroarc region of...
The city of San Juan, in the Central-Western region of Argentina, has been the target of very destru...
Research for evaluation of geologic hazards involving earthquakes and volcanic eruptions in southern...
This paper analyzes the style, distribution, mechanics and timing of deformation of the Andean retro...
The Oligocene to present evolution of the North Patagonian Andes is analyzed linking geological and ...
This chapter focuses on the neotectonics of Argentine–Chilean Patagonia and overviews the active tec...
The Cenozoic tectonic evolution of the North Patagonian Andes is analyzed linking geological and geo...
Twenty-five new long-period magnetotelluric sites near 31.5°S were collected in a west–east profile....
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
This study shows the neotectonic deformation occurred in the southern piedmont of the Cumbres Calcha...
The eastern Sierras Pampeanas (ESP) are the easternmost expression of a series of foreland uplifts i...
At the northern sector of the Precordillera Sur (31° 50′-32° 40′ SL/68° 45′-69° 20′ WL), Central And...
The Guacha Corral shear zone (GCSZ) is represented by mylonites that were developed under amphibolit...
The Sierras Pampeanas of Córdoba are the easternmost uplifted blocks caused by Andean foreland defor...