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Sr and Nd isotope variations along the Pleistocene San Pedro - linzor volcanic chain, N. Chile: tracking the influence of the upper crustal altiplano puna magma body
(Elsevier, 2017)
Subduction-related magmas that erupted in the Central Andes during the past 10 Ma are strongly affected by crustal assimilation as revealed by an increase in Sr-87/Sr-86 isotope ratios with time that in turn are correlated ...
Synthesis: PLUTONS: Investigating the relationship between pluton growth and volcanism in the Central Andes
(Geological Society of America, 2018-06)
The Central Andes is a key global location to study the enigmatic relation between volcanism and plutonism because it has been the site of large ignimbrite-forming eruptions during the past several million years and currently ...
Constraining the sub-arc, parental magma composition for the giant Altiplano-Puna Volcanic Complex, northern Chile
(Nature, 2020)
The Andean continental arc is built upon the thickest crust on Earth, whose eruption products reflect varying degrees of crustal assimilation. In order to robustly model magma evolution and assimilation at subduction zones ...
Evolución geológica del Volcán Azufre II Región de Antofagasta
(Universidad de Chile, 2018)
El Volcán Azufre es uno de los estratovolcanes que componen la Zona Volcánica Central de Los Andes, perteneciendo en particular al borde occidental del Altiplano Puna Volcanic Complex (APVC). Esta región ubicada en el ...
Modelamiento tridimensional del sistema volcánico Paniri-Toconce, mediante el uso de magnetotelúrica
(Universidad de Chile, 2018)
The research is located in the San Pedro-Toconce volcanic chain in the central volcanic zoneof the Andes, North Chile. This area is interesting because of its proximity to several active volcanic centers, the geysers field ...