Volcanism and metamorphism are the principal geologic processes that drive carbon transfer from the interior of Earth to the surface reservoir. 1–4 Input of carbon to the surface …
Earth degassing of CO2-rich fluids has been proven to contribute significantly to the global carbon budget. The presence of ubiquitous outgassing reveals some degree of permeability …
To investigate the underlying magmatic systems that drive high-temperature geothermal fields and volcanism in the north-central Taupo Volcanic Zone (TVZ), we use a combination …
Here we report on the first assessment of volatile fluxes from the hyperacid crater lake hosted within the summit crater of Copahue, a very active volcano on the Argentina‐Chile …
Magnetotelluric data were recorded in a 45× 10 km band crossing the Rotorua and Waimangu geothermal fields in the northern part of the Taupo Volcanic Zone in the central …
We investigate the geological and hydrothermal setting at Lake Rotomahana, using recently collected potential-field data, integrated with pre-existing regional gravity and aeromagnetic …
Volcanic lakes in large silicic caldera volcanoes are an important source of CO 2 emissions. However, quantifying CO 2 output is challenging due to the lack of observed historical CO 2 …
Risk mitigation in long-dormant volcanic provinces is a challenge due to the absence of collective memory of past disasters as well as the scarcity, and subtlety, of unrest signals that …
There are hundreds of volcanic lakes around the world that represent an important hazard due to the potential occurrence of phreatomagmatic or limnic eruptions. Variations in …