Subduction zones represent the interface between Earth's interior (crust and mantle) and exterior (atmosphere and oceans), where carbon and other volatile elements are actively …
Volcanic lakes carry fluids that range from ultra acid, high TDS brines to largely meteoric fluids. Their water compositions are governed by volcanic fluid inputs, which range from …
Volcanic acid sulfate–chloride brines form through absorption of volcanic vapors in shallow reservoirs of meteoric water. Reaction with surrounding volcanic rocks leads to partial …
Copahue volcano is part of the Caviahue–Copahue Volcanic Complex (CCVC), which is located in the southwestern sector of the Caviahue volcano-tectonic depression (Argentina …
N Søager, PM Holm, EJ Llambías - Chemical Geology, 2013 - Elsevier
The Pleistocene to Holocene Payenia volcanic province is a backarc region of 60,000 km2 in Mendoza, Argentina, which is dominated by transitional to alkaline basalts and …
MC Ray, DR Hilton, J Muñoz, TP Fischer, AM Shaw - Chemical Geology, 2009 - Elsevier
We report new helium and carbon isotope (3He/4He, δ13C) and relative abundance (CO2/3He) characteristics of a suite of hydrothermal gases and fluids (fumaroles, hot …
Four earthquakes with Mw≥ 8 occurred in proximity to 60 Holocene volcanoes, in the Southern Volcanic Zone of the Andes (SVZ) since 1906. We analyzed these events by …
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 …
MA Giaveno, MS Urbieta, JR Ulloa, E González Toril… - Microbial ecology, 2013 - Springer
A novel thermoacidophilic archaeal strain has been isolated from three geothermal acidic hot springs in Copahue, Argentina. One of the most striking characteristic of ALE1 isolate is …