Pyroclastic and lava vent-facies, from the Late Jurassic El Quemado Complex, are described at the southern Lake Ghío, in the Cordillera Patagónica Austral. Based on the comprehensive study of lithology and structures, the reconstruction of the volcanic architecture has been carried out. Four ignimbrites and one rhyolitic lava unit, affected by oblique-slip normal faults have been recognized. The evolution of La Peligrosa Caldera has been modeled in three different stages:1) initial collapse, consisting of a precursory downsag subsidence, related to a dilatational zone, which controlled the location of the caldera, 2) main collapse, with the emplacement of large volume crystal-rich ignimbrites and megabreccias, under a progressive subsidence...
The volcano-sedimentary succession of the Cerro Piche Graben, Río Negro province, Patagonia (Argenti...
We analyse the volcanic stratigraphy of the Lower Jurassic synrift sequence of the Sañicó depocentre...
The long-lived La Hoyada Volcanic Complex (LHVC) is located in the east of Cordillera de San Buenave...
Two compositionally different volcanic cycles are documented by geological mapping, lithofacies and ...
The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North...
The Coranzulí caldera (23°00′ S – 66°15′ W) is one of the least known caldera complexes in the easte...
The Payún Matrú caldera is a Quaternary Andean back-arc caldera (36° 25′ S, 69° 12′ 30? W), and repr...
The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif,exhibits...
A partir del levantamiento aeromagnético del Macizo del Deseado, se ha podido interpretar la presenc...
The magmatic record of the North Patagonian Batholith starts in Middle Jurassic times and rapidly gr...
Volcanism at Sierra del Morro represents the final stages of the flat-slab related magmatism in the ...
One of the largest silicic igneous provinces of the world, the Chon Aike Volcanic Province, is relat...
This article identifies the Pucarilla–Cerro Tipillas Volcanic Complex and its major eruptive source,...
A late Early Jurassic shortening event affected the southern end of the back-arc Chubut Basin in sou...
The Quaternary Payún Matrú volcano is a long-lived edifice that developed a summit caldera 8 km wide...
The volcano-sedimentary succession of the Cerro Piche Graben, Río Negro province, Patagonia (Argenti...
We analyse the volcanic stratigraphy of the Lower Jurassic synrift sequence of the Sañicó depocentre...
The long-lived La Hoyada Volcanic Complex (LHVC) is located in the east of Cordillera de San Buenave...
Two compositionally different volcanic cycles are documented by geological mapping, lithofacies and ...
The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North...
The Coranzulí caldera (23°00′ S – 66°15′ W) is one of the least known caldera complexes in the easte...
The Payún Matrú caldera is a Quaternary Andean back-arc caldera (36° 25′ S, 69° 12′ 30? W), and repr...
The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif,exhibits...
A partir del levantamiento aeromagnético del Macizo del Deseado, se ha podido interpretar la presenc...
The magmatic record of the North Patagonian Batholith starts in Middle Jurassic times and rapidly gr...
Volcanism at Sierra del Morro represents the final stages of the flat-slab related magmatism in the ...
One of the largest silicic igneous provinces of the world, the Chon Aike Volcanic Province, is relat...
This article identifies the Pucarilla–Cerro Tipillas Volcanic Complex and its major eruptive source,...
A late Early Jurassic shortening event affected the southern end of the back-arc Chubut Basin in sou...
The Quaternary Payún Matrú volcano is a long-lived edifice that developed a summit caldera 8 km wide...
The volcano-sedimentary succession of the Cerro Piche Graben, Río Negro province, Patagonia (Argenti...
We analyse the volcanic stratigraphy of the Lower Jurassic synrift sequence of the Sañicó depocentre...
The long-lived La Hoyada Volcanic Complex (LHVC) is located in the east of Cordillera de San Buenave...