The Andean volcanic arc includes over 200 potentially active Quaternary volcanoes, and at
least 12 giant caldera/ignimbrite systems, occurring in four separate segments referred to as …

Abstract The Andes of the Neuquén region (36°− 38° S latitude) of the Central Andes have
distinctive characteristics that result from the alternation of periods of generalized extension …

The 1960 rhyodacitic fissure eruption in the Cordón Caulle Volcanic Complex (CCVC),
located in Southern Andes (40.5° S) was a unique volcanic episode. The remarkable …

We modelled the transport and deposition of ash from the June 2011 eruption from Cordón
Caulle volcanic complex, Chile. The modelling strategy, currently under development at the …

Patterns of spatial distribution, and geochemical and isotopic evolution from subduction-
related igneous rocks provide tools for scaling, balancing and predicting orogenic processes …

The nature of the relationship between tectonics and volcanism in a specific area is the
result of the interaction between the crustal structures of the basement and ongoing regional …

This paper describes the volcanostratigraphy, structure, and tectonic implications of an arc
volcanic complex in an oblique subduction setting: the Caviahue caldera Copahue volcano …

Abstract The Chos Malal and Agrio fold and thrust belts are located in the western part of the
Neuquén basin, an Andean retroarc basin of central-western Argentina. Both belts show …

In this contribution we address the current controversial issues related to the age,
correlation, tectonic setting and paleogeographic links of the Cenozoic fossiliferous marine …

The Northern Patagonian Andes have been constructed through multiple mechanisms that
range from tectonic inversion of extensional structures of Early to Middle Jurassic age in the …