Tephrochronology studies the deposits of explosive volcanic eruptions in the stratigraphic
record. The Southern (SVZ, 33–46° S) and Austral (AVZ, 49–55° S) Volcanic Zones of the …

Few studies along the western slopes of the Andes in Northwestern Patagonia (NWP: 40°-
44° S) allow examining vegetation development through environmental gradients in latitude …

The chemistry of erupted clinopyroxene crystals (±equilibrium liquids) have been widely
used to deduce the pressures and temperatures of magma storage in volcanic arcs …

The origin of gaps or zoning in the composition of erupted products is critical to
understanding how sub-volcanic reservoirs operate. We characterize the compositionally …

We describe the stratigraphy, age, geochemistry and correlation of tephra from west to east
across the northern Patagonian Andes (c. 40–41° S) with a view to further refining the …

Determining how and why eruptive outputs are modulated by the loading and unloading of
ice is key to understanding whether ongoing and accelerating deglaciation across mid-to …

We present results from Lago Negro, a small closed-basin lake adjacent to Lago Rosselot,
to examine the vegetation and environmental history of an insufficiently studied sector of …

Lanín is a composite volcano (∼ 39.38° S; 71.30° W) located in the Central Southern
Volcanic Zone of the Andes. It is the southernmost member of the NW-SE volcanic alignment …

Understanding the relationship between crustal faults and volcanic activity in
transpressional environments is a main goal in geosciences and could help to understand …

Determining the eruption frequency-Magnitude (fM) relationship for data-limited volcanoes is
challenging since it requires a comprehensive eruption record of the past eruptive activity …