Igneous origin of Co₂ in ancient and recent hot-spring waters and travertines from the northern argentinean andes

Keyphrases

• Water Availability 100%
• Dissolved Inorganic Carbon 100%
• Andes 100%
• Hot Spring Water 100%
• Igneous Origin 100%
• Hydrothermal System 66%
• Carbonate 66%
• Late Pleistocene 66%
• Volcanic Activity 66%
• Aragonite 66%
• Altiplano 66%
• CO2 Sources 66%
• Large Lakes 33%
• Heat Flux 33%
• Ponds 33%
• Manganese Oxide 33%
• Humid Climate 33%
• Iron Oxide 33%
• CO2 Flux 33%
• CO 2 33%
• Isotopic Signature 33%
• Climatic Change 33%
• Fault Zone 33%
• Carbon 13C 33%
• CO2 Supply 33%
• Inorganic Carbon Source 33%
• Mineralogy 33%
• Marine Isotope Stages 33%
• Deep-seated 33%
• Hydrothermal Activity 33%
• Fluid Inclusions 33%
• Water-rock 33%
• Highstand 33%
• Organic Matter Degradation 33%
• Regional Factors 33%
• Thermal Water 33%
• Water Salinity 33%
• Hydrodynamic Uncertainty 33%
• Climate Period 33%
• Petrographic Features 33%
• Igneous Processes 33%
• CO2 Sink 33%
• Process Activity 33%
• CO2 Budget 33%
• Central Andes 33%
• Pseudomorph 33%
• Thermalism 33%
• Feature Signatures 33%
• Thermal Systems 33%
• Deep-seated Faults 33%
• Carbonate Precipitates 33%
• Precipitation Water 33%
• Humid Period 33%
• Marine Isotope Stage 9 33%

Earth and Planetary Sciences

• Andes 100%
• Travertine 100%
• Thermal Spring 100%
• Spring Water 100%
• Carbon Dioxide 50%
• Water Availability 25%
• Dissolved Inorganic Carbon 25%
• Hydrothermal System 16%
• Calcite 16%
• Late Pleistocene 16%
• Aragonite 16%
• Climate Change 8%
• Mineralogy 8%
• Iron Oxide 8%
• Fault Zone 8%
• Marine Isotope Stage 8%
• Hydrothermal Activity 8%
• Fluid Inclusion 8%
• Water Salinity 8%
• Thermal Water 8%
• Pseudomorph 8%
• Emissions 8%
• Organic Matter 8%
• Manganese Oxide 8%
• Heat Flux 8%