Chemical and isotopic features of cold and thermal fluids discharged in the Southern Volcanic Zone between 32.5°S and 36°S: Insights into the physical and chemical processes controlling fluid geochemistry in geothermal systems of Central Chile
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文摘

Two areas showing fluids with different geochemical features were recognized.

Mature NaCl waters only occurred in the eastern area close to the volcanic chain.

Local and regional tectonics control the spatial distribution of the thermal springs.

Fluids geochemistry mostly depends on the lithology of rocks interacting with waters.

Fluids associated with active volcanoes equilibrate at temperatures up to 300 °C.

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