The Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-54°S is part of a poorly studied hinterland region of the southernmost Andean Cordillera. This domain consists of NNW-SSE trending tectonic slices of pre-Jurassic basement units and Upper Jurassic-Lower Cretaceous ophiolitic complexes and volcano-sedimentary successions of the Rocas Verdes Basin (RVB). New detrital zircon U–Pb ages of metatuffs and metapsammopelites constrain episodes of Late Jurassic rift-related volcanism (ca. 160 Ma) followed by Early Cretaceous sedimentation (ca. 125 Ma) during the opening of the RVB. Shear bands developed in the RVB units further record the initial phases of the Andean Orogeny. The 30-km wide thrust stack located on top of the...
This study synthesizes the tectonomagmatic evolution of the Andes between 35°30′S to 48°S with the a...
The Cretaceous-Cenozoic evolution of the Patagonian broken foreland basin system at 42–43°S in the n...
Comprehensive knowledge on the tempo and style of shortening, exhumation, and sedimentary evolution ...
The hinterland Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-54°S is part...
The Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-54°S is part of a poorl...
New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationshi...
Orientador: Prof. Dr. Leonardo Fadel CuryCoorientador: Prof. Dr. Mauricio CalderónDissertação (mestr...
textThe southern Patagonian Andes record the Late Cretaceous closure and inversion of the Late Juras...
The combination of detrital low-temperature thermochronology with previous U–Pb geochronology, petro...
In this study, we propose a geodynamic model covering sedimentation, metamorphism, magmatism, and ex...
We studied the northern tip of the Austral-Magallanes basin in the Southern Patagonian Andes, betwee...
The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique collision of the Pale...
Decoding the earliest orogenic stages in the Andes, the largest subduction orogen on Earth is fundam...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
The Cordillera de los Andes is the typical example of a subduction-related orogen. Its present topog...
This study synthesizes the tectonomagmatic evolution of the Andes between 35°30′S to 48°S with the a...
The Cretaceous-Cenozoic evolution of the Patagonian broken foreland basin system at 42–43°S in the n...
Comprehensive knowledge on the tempo and style of shortening, exhumation, and sedimentary evolution ...
The hinterland Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-54°S is part...
The Western Domain of the Magallanes Fold-and-Thrust Belt (MFTB) between 52°-54°S is part of a poorl...
New detailed structural data from the Fuegian Andes including new ages and cross-cutting relationshi...
Orientador: Prof. Dr. Leonardo Fadel CuryCoorientador: Prof. Dr. Mauricio CalderónDissertação (mestr...
textThe southern Patagonian Andes record the Late Cretaceous closure and inversion of the Late Juras...
The combination of detrital low-temperature thermochronology with previous U–Pb geochronology, petro...
In this study, we propose a geodynamic model covering sedimentation, metamorphism, magmatism, and ex...
We studied the northern tip of the Austral-Magallanes basin in the Southern Patagonian Andes, betwee...
The Pampean orogeny of northern Argentina resulted from Early Cambrian oblique collision of the Pale...
Decoding the earliest orogenic stages in the Andes, the largest subduction orogen on Earth is fundam...
The Southern Patagonian Andes (SPA)between 47°?48°S are characterized by relatively high elevations ...
The Cordillera de los Andes is the typical example of a subduction-related orogen. Its present topog...
This study synthesizes the tectonomagmatic evolution of the Andes between 35°30′S to 48°S with the a...
The Cretaceous-Cenozoic evolution of the Patagonian broken foreland basin system at 42–43°S in the n...
Comprehensive knowledge on the tempo and style of shortening, exhumation, and sedimentary evolution ...