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This study characterizes the hydrogeochemistry of hot springs in the Andes of Ecuador, resulting from volcanic activity due to the subduction of the Nazca plate. Two groups of geothermal waters were identified: one associated with extinct volcanic activity (Na+-Cl- type) and another linked to young Quaternary volcanic activity (Mg2+-HCO3-, Na+-HCO3-, Na+-SO42-, Mg2+-SO42- types). The research utilized various hydrochemical diagrams to analyze water samples and their relationship with Ecuador

Author

alvaroacardonag

Language

EN