Copahue volcano straddling the edge of the Agrio‐Caviahue caldera along the Chile‐
Argentina border in the southern Andes has been in unrest since inflation began in late …

Dike swarms are the fossil remains of regions of the crust that have undergone repeated
magma injections. Volcanic earthquake swarms and geodetic measurements are, at least in …

The Copahue volcano host one of the most attractive geothermal resources of Argentina.
Several studies focused on both the volcanic activity and the related geothermal …

Understanding interactions between tectonic faults and a nearby active volcano is often
realized by combining seismic and field observations. A good example of such an …

The volcano-hosted geothermal system of Copahue is one of the most promising resources
of renewable energy in Argentina. The associated geothermal field is bounded by a set of …

An exhaustive review of the available data related to the reservoir of the volcano-hosted
Copahue geothermal system is presented. Reservoir interpretation to date suggests a vapor …

Improving the ability to detect and characterize long-duration volcanic tremor is crucial to
understand the long-term dynamics and unrest of volcanic systems. We have applied data …

Abstract The Caviahue-Copahue Volcanic Complex (CCVC, 37° 51'S-71° 05′ W) is located
in the central segment of the South Volcanic Zone,~ 30 km eastward from the main Andean …

Improving the ability to detect and characterize long-duration volcanic tremor is crucial to
understand the long-term dynamics and unrest of volcanic systems. We have applied data …