The Guacha Corral shear zone (GCSZ) is represented by mylonites that were developed under amphibolites facies conditions from migmatitic protoliths. In this contribution, geophysical, petrological and structural data were combined to determine the 3D geometry of the GCSZ. New gravimetric, magnetometric and structural studies, along an E-W profile, were integrated with existing magnetotelluric and seismological data from a representative regional database of the Eastern Sierras Pampeanas. The zonation of different fabrics across the GCSZ suggests that the pre-existing heterogeneities of the protoliths played a key role in governing the degree of metamorphism of different regions. The low gravity anomalies observed in the GCSZ suggest a trans...
This research is based on a joint geological and geophysical study performed in the South Central An...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
In this paper, the evolution of the fabric and 3D geometry of the Calmayo trondhjemitic pluton (512....
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
Twenty-five new long-period magnetotelluric sites near 31.5°S were collected in a west–east profile....
This paper presents the results of a geophysical study of the southern portion of the Sierra Grande ...
Magnetic fabric patterns and microstructures of granitic rocks provide evidence of structural modifi...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
The main objective of this research is to recognize several geological structures associated with th...
We provide the first modern description of the Cuesta de Randolfo shear zone based on a combination ...
We describe a 1 km-thick ultramylonite forming the high strain base of the >3.5 km-thick El Pichao s...
This study provides new insights about mechanisms of synkinematic interplay between dyking emplaceme...
The evolution of the Paleozoic Claromecó Basin is intimately related to contemporaneous tectonic eve...
The granulite-complexes of the Sierras de Córdoba, inside context of Sierras Pampeanas, expose the d...
This research is based on a joint geological and geophysical study performed in the South Central An...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...
In this paper, the evolution of the fabric and 3D geometry of the Calmayo trondhjemitic pluton (512....
The Nazca Plate subducting beneath the South American Plate, has strongly influenced Cenozoic-mounta...
Twenty-five new long-period magnetotelluric sites near 31.5°S were collected in a west–east profile....
This paper presents the results of a geophysical study of the southern portion of the Sierra Grande ...
Magnetic fabric patterns and microstructures of granitic rocks provide evidence of structural modifi...
New petrologic, thermobarometric and U-Pb monazite geochronologic information allowed to resolve the...
The main objective of this research is to recognize several geological structures associated with th...
We provide the first modern description of the Cuesta de Randolfo shear zone based on a combination ...
We describe a 1 km-thick ultramylonite forming the high strain base of the >3.5 km-thick El Pichao s...
This study provides new insights about mechanisms of synkinematic interplay between dyking emplaceme...
The evolution of the Paleozoic Claromecó Basin is intimately related to contemporaneous tectonic eve...
The granulite-complexes of the Sierras de Córdoba, inside context of Sierras Pampeanas, expose the d...
This research is based on a joint geological and geophysical study performed in the South Central An...
This thesis investigated the evolution of a high temperature, low pressure crustal block of the Late...
The evolution of the western margin of South America comprised different tectonic regimes responsibl...