Hypogenic caves of Syracuse area, Sicily (Italy): geomorphological evidence of CO₂ degassing, fresh-salt water mixing, and late condensation corrosion

Keyphrases

• Italy 100%
• Fluid Mixing 100%
• Syracuse 100%
• CO2 Degassing 100%
• Hypogenic 100%
• Condensation Corrosion 100%
• Hypogenic Caves 100%
• Marine Terraces 66%
• Stable Isotopes 33%
• Sand 33%
• Allogeneic 33%
• Carbon Dioxide 33%
• Stable Isotope Technique 33%
• Degassing 33%
• Speleothem 33%
• Surface Runoff 33%
• Phosphate 33%
• Organic Carbon 33%
• Sulfuric Acid 33%
• Acidification 33%
• Mn Oxides 33%
• Paleomagnetism 33%
• Aggressiveness 33%
• CO2 Concentration 33%
• Shallow Depth 33%
• Ascending Flow 33%
• Seepage 33%
• Mixing Zone 33%
• Kaolinite 33%
• Corrosion Process 33%
• U-Th 33%
• Dating Methods 33%
• Water Table 33%
• Mineralogy 33%
• Marine Notches 33%
• Montmorillonite 33%
• Position Level 33%
• Calcarenite 33%
• Reliability Calculation 33%
• Fe Oxides 33%
• Phreatic 33%
• Deep Sources 33%
• Cave Sediments 33%
• Spar 33%
• Aggressivity 33%
• Bat Guano 33%
• In Situ Weathering 33%
• Hydrothermal Origin 33%
• Cave Morphology 33%
• Eastern Sicily 33%
• Freshwater Lens 33%
• Flank Margin Caves 33%
• Hypogene Speleogenesis 33%

Earth and Planetary Sciences

• Italy 100%
• Carbon Dioxide 100%
• Degassing 100%
• Marine Terrace 66%
• Stable Isotope 66%
• Mineralogy 33%
• Speleothem 33%
• Pleistocene 33%
• Calcite 33%
• Sea Level 33%
• Sulphuric Acid 33%
• Dating Method 33%
• Water Table 33%
• Montmorillonite 33%
• Kaolinite 33%
• Calcarenite 33%
• Morphology 33%
• Paleomagnetism 33%
• Organic Carbon 33%
• Clay Mineral 33%