The Marifil Volcanic Complex is an extended volcanic and pyroclastic unit outcropping in the North Patagonia. It has been included in the Chon Aike large igneous province associated to the thermal anomaly of the Karoo plume. The Marifil Volcanic Complex is mainly composed of rhyolites, dacites, rhyodacites and minor trachytes and trachyandesites. The latter are common in the base of the unit. The upper acidic rocks have been dated between 192 Ma to 151 Ma (Early to Middle Jurassic) by K-Ar, Ar-Ar and Rb-Sr methods. On the other hand, the age of the mesosilicic rocks range from 221 Ma to 173 Ma (K-Ar whole rock ages).In this research, we revise the stratigraphic relations, geochemistry and petrography of the mesosilisic rocks from Marifil Vo...
One of the largest silicic igneous provinces of the world, the Chon Aike Volcanic Province, is relat...
The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern...
Central Patagonia is traversed by a belt of Early to Middle Jurassic calc-alkaline intermediate volc...
Permo-Triassic magmatism is widespread in the eastern North Patagonian Massif and has been related t...
We present the first study of the volcanic rocks of the Cañadón Asfalto Formation that host the Navi...
The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North...
The Los Menucos Complex (northern Patagonia) consists of ∼6 km thick succession of acidic and interm...
The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif,exhibits...
The mid-Jurassic Marifil and Chon-Aike volcanic rocks of eastern Patagonia are part of one of the la...
Two compositionally different volcanic cycles are documented by geological mapping, lithofacies and ...
Permo-Triassic magmatism is widespread in the eastern North Patagonian Massif and has been related t...
This contribution deals first new ICP-MS U–Pb zircon ages that indicate Middle- and Late Triassic ma...
The Upper Triassic magmatic and tectonic evolution of the central North Patagonian Massif is evaluat...
We present the first geochronologically constrained igneous stratigraphy of the Permian to Early Tri...
The Marifil Volcanic Complex, exposed in the eastern North Patagonian Massif, Argentina, includes up...
One of the largest silicic igneous provinces of the world, the Chon Aike Volcanic Province, is relat...
The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern...
Central Patagonia is traversed by a belt of Early to Middle Jurassic calc-alkaline intermediate volc...
Permo-Triassic magmatism is widespread in the eastern North Patagonian Massif and has been related t...
We present the first study of the volcanic rocks of the Cañadón Asfalto Formation that host the Navi...
The Sinemurian Marifil Volcanic Complex at Sierra de Pailemán, located in the east part of the North...
The Los Menucos Complex (northern Patagonia) consists of ∼6 km thick succession of acidic and interm...
The northern zone of the Chon Aike Igneous Province, located in the North Patagonian Massif,exhibits...
The mid-Jurassic Marifil and Chon-Aike volcanic rocks of eastern Patagonia are part of one of the la...
Two compositionally different volcanic cycles are documented by geological mapping, lithofacies and ...
Permo-Triassic magmatism is widespread in the eastern North Patagonian Massif and has been related t...
This contribution deals first new ICP-MS U–Pb zircon ages that indicate Middle- and Late Triassic ma...
The Upper Triassic magmatic and tectonic evolution of the central North Patagonian Massif is evaluat...
We present the first geochronologically constrained igneous stratigraphy of the Permian to Early Tri...
The Marifil Volcanic Complex, exposed in the eastern North Patagonian Massif, Argentina, includes up...
One of the largest silicic igneous provinces of the world, the Chon Aike Volcanic Province, is relat...
The Andesitas Alvar Formation is part of the large Jurassic volcanic province of Patagonia (southern...
Central Patagonia is traversed by a belt of Early to Middle Jurassic calc-alkaline intermediate volc...