The Coranzulí caldera (23°00′ S ? 66°15′ W) is one of the least known caldera complexes in the eastern part of the Argentinian Altiplano-Puna plateau (Central Andes). It lies at the intersection of N S, NW-SE and NE-SW fault systems and was formed about 6.6Ma ago; during the eruption, four main crystal-rich daciticignimbrites were emplaced in different directions around the caldera. Caldera collapse was not homogeneous, rather it occurred along different sectors of the ring fault as subsidence progressed. The location of co-ignimbrite lag breccias and the composition of the dominant lithic fragments within the different ignimbrite flow units reveal how the caldera collapse developed. According to the succession of deposits, in particular th...
Collapse calderas are defined as the volcanic depression that result from the disruption of the geom...
Two main stages are distinguished in the evolution of the Diamante Caldera-Maipo volcano complex. Th...
Central (18–28° S) and Southern (33–46° S) Andean Volcanic Zones (CVZ and SVZ, respectively) have se...
The Coranzulí caldera (23°00′ S – 66°15′ W) is one of the least known caldera complexes in the easte...
We present a detailed stratigraphy of the Coranzulí caldera-forming deposits. This caldera, located ...
The Payún Matrú caldera is a Quaternary Andean back-arc caldera (36° 25′ S, 69° 12′ 30? W), and repr...
This article identifies the Pucarilla–Cerro Tipillas Volcanic Complex and its major eruptive source,...
A new emission center of extensive pyroclastic flows has been recognized and interpreted, near San A...
Graduation date: 2014The Pastos Grandes Caldera Complex (PGCC) in southwest Bolivia has produced two...
In the Cerro Carro Quebrado and Cerro Catri Cura area, located at the border between the Neuquén Bas...
Pyroclastic and lava vent-facies, from the Late Jurassic El Quemado Complex, are described at the so...
Caldera-forming volcanic eruptions are among the most dangerous, and can generate extensive pyroclas...
Caldera-forming volcanic eruptions are among the most dangerous, and can generate extensive pyroclas...
The 35 × 20 km Cerro Galán resurgent caldera is the largest post-Miocene caldera so far identified i...
Explosive volcanism in the Altiplano-Puna Volcanic Zone (APVZ) of the South American Central Andes f...
Collapse calderas are defined as the volcanic depression that result from the disruption of the geom...
Two main stages are distinguished in the evolution of the Diamante Caldera-Maipo volcano complex. Th...
Central (18–28° S) and Southern (33–46° S) Andean Volcanic Zones (CVZ and SVZ, respectively) have se...
The Coranzulí caldera (23°00′ S – 66°15′ W) is one of the least known caldera complexes in the easte...
We present a detailed stratigraphy of the Coranzulí caldera-forming deposits. This caldera, located ...
The Payún Matrú caldera is a Quaternary Andean back-arc caldera (36° 25′ S, 69° 12′ 30? W), and repr...
This article identifies the Pucarilla–Cerro Tipillas Volcanic Complex and its major eruptive source,...
A new emission center of extensive pyroclastic flows has been recognized and interpreted, near San A...
Graduation date: 2014The Pastos Grandes Caldera Complex (PGCC) in southwest Bolivia has produced two...
In the Cerro Carro Quebrado and Cerro Catri Cura area, located at the border between the Neuquén Bas...
Pyroclastic and lava vent-facies, from the Late Jurassic El Quemado Complex, are described at the so...
Caldera-forming volcanic eruptions are among the most dangerous, and can generate extensive pyroclas...
Caldera-forming volcanic eruptions are among the most dangerous, and can generate extensive pyroclas...
The 35 × 20 km Cerro Galán resurgent caldera is the largest post-Miocene caldera so far identified i...
Explosive volcanism in the Altiplano-Puna Volcanic Zone (APVZ) of the South American Central Andes f...
Collapse calderas are defined as the volcanic depression that result from the disruption of the geom...
Two main stages are distinguished in the evolution of the Diamante Caldera-Maipo volcano complex. Th...
Central (18–28° S) and Southern (33–46° S) Andean Volcanic Zones (CVZ and SVZ, respectively) have se...